TY - CHAP A1 - Hirsch, Jens T1 - Die Rolle der Kommunen - das Beispiel der Mittelstädte T2 - Handelsimmobilien - Theoretische Ansätze, empirische Ergebnisse N2 - No abstract available. KW - Einzelhandel KW - Kommune KW - Mittelstädte KW - Einzelhandelsentwicklung Y1 - 2013 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-182602 PB - Verlag MetaGIS Infosysteme CY - Mannheim ER - TY - JOUR A1 - Meister, Julia A1 - Lange-Athinodorou, Eva A1 - Ullmann, Tobias T1 - Preface: Special Issue “Geoarchaeology of the Nile Delta” JF - E&G Quarternary Science Journal N2 - No abstract available. KW - geoarcheology Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-261195 VL - 70 ER - TY - JOUR A1 - Riyas, Moidu Jameela A1 - Syed, Tajdarul Hassan A1 - Kumar, Hrishikesh A1 - Kuenzer, Claudia T1 - Detecting and analyzing the evolution of subsidence due to coal fires in Jharia coalfield, India using Sentinel-1 SAR data JF - Remote Sensing N2 - Public safety and socio-economic development of the Jharia coalfield (JCF) in India is critically dependent on precise monitoring and comprehensive understanding of coal fires, which have been burning underneath for more than a century. This study utilizes New-Small BAseline Subset (N-SBAS) technique to compute surface deformation time series for 2017–2020 to characterize the spatiotemporal dynamics of coal fires in JCF. The line-of-sight (LOS) surface deformation estimated from ascending and descending Sentinel-1 SAR data are subsequently decomposed to derive precise vertical subsidence estimates. The most prominent subsidence (~22 cm) is observed in Kusunda colliery. The subsidence regions also correspond well with the Landsat-8 based thermal anomaly map and field evidence. Subsequently, the vertical surface deformation time-series is analyzed to characterize temporal variations within the 9.5 km\(^2\) area of coal fires. Results reveal that nearly 10% of the coal fire area is newly formed, while 73% persisted throughout the study period. Vulnerability analyses performed in terms of the susceptibility of the population to land surface collapse demonstrate that Tisra, Chhatatanr, and Sijua are the most vulnerable towns. Our results provide critical information for developing early warning systems and remediation strategies. KW - coal fire KW - InSAR KW - subsidence KW - remote sensing KW - coal KW - interferometry KW - SBAS Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-236703 SN - 2072-4292 VL - 13 IS - 8 ER - TY - THES A1 - Mann, Daniel T1 - "The smell of Ujamaa is still there" - Tanzania’s Path of Development between Grassroots Socialism and Central State Control in Ruvuma N2 - In the 1960s, when most African nations gained their independence after the age of colonialism, several theories and strategies emerged with the goal of "developing" these apparently "underdeveloped" territories. One of the most influential approaches for this task was represented in Julius K. Nyerere´s idea of Ujamaa, the Tanzanian version of African socialism. Even before the Arusha Declaration established Ujamaa as a national development strategy in 1967, several groups of politicized young farmers took to the empty countryside of Tanzania to implement their own version of cooperative development. From one of these attempts emerged the Ruvuma Development Association (RDA), which organized up to 18 villages in southwestern Tanzania. The RDA became the inspiration for Nyerere´s concretization of Ujamaa and its implementation on national level. Yet, the central state could not replicate the success of the peasants, which was based on voluntariness and intrinsic motivation. In 2015, this exploratory study has revisited the Region of Ruvuma. Through a case study approach, relying mostly on qualitative methods, new insights into the local history of Ujamaa and its perception have been gathered. In particular, narrative interviews with contemporary witnesses and group interviews with the present-day farmers’ groups have been conducted. Furthermore, NGOs active within the region, as well as regional and local government institutions were among the key stakeholders identified to concretize the local narrative of Ujamaa development. All interviews were analyzed according to the principles of qualitative content analysis. Additionally, individual villager questionnaires were used to achieve a more holistic picture of the local perception of development, challenges and the Ujamaa era. None of the original Ujamaa groups of the times of the RDA was still operational at the time of research and no case of village-wide organization of collective agriculture could be observed. Nevertheless, in all of the three case study villages, several farmers’ groups (vikundi) were active in organizing development activities for their members. Furthermore, the perception of the Ujamaa era was generally positive throughout all of the case study sites. Yet, there have been significant differences in this perception, based on the village, age, gender and field size of the recipients. Overall, the period of Ujamaa was seen as an inspiration for present-day group activities, and the idea of such activities as a remedy for the developmental challenges of these villages was common among all stakeholders. This thesis concludes that the positive perception of group activities as a vehicle for village development and the perception of Ujamaa history as a positive asset for the inception and organization of farmers’ groups would be highly beneficial to further attempts to support such development activities. However, the limitations in market access and capital availability for these highly-motivated group members have to be addressed by public and private development institutions. Otherwise, "the smell of Ujamaa" will be of little use for the progress of these villages. N2 - In den 1960er Jahren, als die meisten Nationen Afrikas ihre Unabhängigkeit erlangten, entstanden etliche Strategien und Theorien, welche die "Entwicklung" dieser „unterentwickelten“ Territorien zum Ziel hatten. Einer der einflussreichsten Ansätze für dieses Ziel war Julius K. Nyereres Idee von Ujamaa, der tansanischen Variante des afrikanischen Sozialismus. Noch bevor die Arusha Deklaration Ujamaa 1967 als nationale Entwicklungsstrategie verankerte, versuchten sich verschiedene Gruppen junger, politisierter Bauern an ihrer eigenen Version der kooperativen Entwicklung im dünn besiedelten ländlichen Raum Tansanias. Aus einem dieser Versuche ging die Ruvuma Development Association (RDA) hervor, welche bis zu 18 Dörfer im Südwesten des Landes organisierte. Die RDA wurde die Inspiration für Nyereres Konkretisierung von Ujamaa, sowie dessen Umsetzung auf nationaler Ebene. Allerdings war der Zentralstaat nicht in der Lage, den auf Freiwilligkeit und intrinsischer Motivation beruhenden Erfolg dieser einfachen Bauern zu reproduzieren. Die vorliegende explorative Studie wurde 2015 in der Region Ruvuma durchgeführt und konnte durch einen, im wesentlich auf qualitativen Methoden beruhenden, Case-Study Ansatz neue Einblicke in die lokale Ujamaa-Geschichte sowie deren Wahrnehmung sammeln. Insbesondere wurden narrative Zeitzeugeninterviews und Gruppeninterviews mit heutigen Bauerngruppen durchgeführt. Zur Konkretisierung des lokalen Narratives der Ujamaa Entwicklung wurden zudem in der Region aktive NGOs sowie Regional- und Kommunalverwaltung befragt. Alle Interviews wurden mittels qualitativer Inhaltsanalyse ausgewertet. Zusätzlich dienten, an individuelle Dorfbewohner gerichtete, Fragebögen zur Herausarbeitung eines umfassenden Bildes der lokalen Wahrnehmung von Entwicklung, Herausforderungen und der Ujamaa Ära an sich. Keine der ursprünglichen Ujamaa Gruppen war zum Zeitpunkt der Erhebung noch aktiv. Ebenso konnte kein Fall einer das ganze Dorf umfassenden kollektiven Landwirtschaft beobachtet werden – kleinere Bauerngruppen (vikundi) kristallisierten sich dagegen als rezente Form kooperativer Entwicklungsmodelle heraus. Darüber hinaus war die Wahrnehmung der Ujamaa Ära in allen untersuchten Dörfern überwiegend positiv. Jedoch zeigten sich signifikante Unterschiede dieser Wahrnehmung bezüglich des Wohnortes, des Alters, des Geschlechts und der Größe des Feldes der Befragten. Insgesamt wurde die Zeit von Ujamaa als eine Inspiration für heutige gruppenbasierte Entwicklungsaktivitäten gesehen, welche wiederum von allen Akteuren als Möglichkeit zur Überwindung der Entwicklungsprobleme dieser Dörfer gesehen wurden. Diese Dissertation kommt zu dem Schluss, dass die positive Wahrnehmung von Gruppenaktivitäten als ein Instrument zur kommunalen Entwicklung und die Wahrnehmung der Ujamaa Ära als ein positives "Asset" für die Gründung und Organisation von vikundi sehr vorteilhafte Voraussetzungen für weitere Entwicklungsaktivitäten bieten. Allerdings fehlen diesen Gruppen Kapital und Marktzugang. Dies muss von staatlichen wie nichtstaatlichen Entwicklungsorganisationen angegangen werden, andernfalls wird der "smell of Ujamaa" wenig zum Fortschritt in diesen Dörfern beitragen. T3 - Würzburger Geographische Arbeiten - 121 KW - Ujamaa-Sozialismus KW - Tansania KW - Ruvuma Development Association KW - Entwicklungstheorie KW - Cooperative Development KW - Rural Development Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-154079 SN - 978-3-95826-066-5 (print) SN - 978-3-95826-067-2 (online) SN - 0510-9833 SN - 2194-3656 N1 - Parallel erschienen als Druckausgabe in Würzburg University Press, 978-3-95826-066-5, 31,80 EUR. PB - Würzburg University Press CY - Würzburg ET - 1. Auflage ER - TY - THES A1 - Strauch, Ulrike T1 - Wassertemperaturbedingte Leistungseinschränkungen konventioneller thermischer Kraftwerke in Deutschland und die Entwicklung rezenter und zukünftiger Flusswassertemperaturen im Kontext des Klimawandels N2 - Mit der vorliegenden Arbeit werden konventionelle thermische Kraftwerke an deutschen Flüssen identifiziert, bei denen aufgrund hoher Flusswassertemperaturen im Zusammenhang mit wasserrechtlichen Grenzwerten Leistungseinschränkungen auftraten. Weiterhin wird aufgezeigt, wie sich die Wassertemperaturen der Flüsse in der Vergangenheit (rezent) entwickelt haben und wie sie sich zukünftig im Kontext des Klimawandels entwickeln könnten. Mittels Literaturrecherche, Medienanalyse und schriftlicher Befragung wurden konventionelle thermische Kraftwerke identifiziert, welche wassertemperaturbedingte Leistungseinschränkungen verzeichneten. Die meisten dieser Leistungseinschränkungen zwischen 1976 und 2007 zeigen sich bei großen Kraftwerken mit einer elektrischen Bruttoleistung über 300 Megawatt, bei Steinkohle- und Kernkraftwerken, bei Kraftwerken mit Durchlaufkühlung und bei solchen, die zwischen 1960 und 1990 in Betrieb gingen. Trendanalysen interpolierter und homogenisierter, rezenter Wassertemperaturzeitreihen deutscher Flüsse ergeben positive Trends v. a. im Frühjahr und Sommer. Die Zählstatistik zeigt in den Jahren 1994, 2003 und 2006 die meisten Tage mit sehr hohen und extrem hohen Wassertemperaturen in den Sommermonaten. In diesen Jahren traten gleichzeitig 63 % aller identifizierter wassertemperaturbedingter Leistungseinschränkungen bei Kraftwerken, meist zwischen Juni und August, auf. Für die Trendanalysen und den Mittelwertvergleich simulierter zukünftiger Wassertemperaturzeitreihen wurden drei Szenarien – B1, A1B und A2 sowie drei Zukunftsperioden 2011-2040, 2011/2041-2070, 2011/2071-2100 betrachtet. Es ergeben sich für die Zukunftsperiode 2011-2040 des A1B- oder A2-Szenarios in mindestens einem der Sommermonate eine Erwärmung und für das B1-Szenario negative oder keine Trends. Die mittleren Wassertemperaturen der Zukunftsperiode 2011-2040 zeigen in allen drei Szenarien gegenüber denen der Klimanormalperiode 1961-1990 positive Unterschiede in mindestens einem der Sommermonate. Für die beiden späteren Zukunftsperioden bis 2070 bzw. bis 2100 liegen in allen Wassertemperaturzeitreihen der drei Szenarien im Sommer positive Trends bzw. Differenzen gegenüber den mittleren Wassertemperaturen der Klimanormalperiode vor. Durch die Synthese der drei Analysen ist erkennbar, dass Isar, Rhein, Neckar, Saar, Elbe und Weser die meisten Kraftwerksstandorte mit wassertemperaturbedingten Leistungseinschränkungen verzeichnen. Es zeigen sich hier positive Trends sowohl in den rezenten als auch zukünftigen Wassertemperaturen für die Zukunftsperiode 2011-2040 des A1B- und A2-Szenarios in jeweils mindestens einem der Sommermonate. Gegenüber den mittleren Wassertemperaturen der Klimanormalperiode liegen für alle drei Szenarien positive Unterschiede der Wassertemperaturen vor. Bei einer Kraftwerkslaufzeit von 40-50 Jahren und einem Kernenergieausstieg 2022 bzw. 2034, werden 48-64 % bzw. 67-91 % der Kraftwerke mit wassertemperaturbedingten Leistungseinschränkungen bis 2022 bzw. 2034 außer Betrieb gehen. Bei einer Laufzeitverlängerung würden nach 2022 fünf der elf betroffenen Kernkraftwerke weiter am Netz bleiben. Somit kann es wieder zu wassertemperaturbedingten Leistungseinschränkungen kommen. In Deutschland sind nach wie vor große Kraftwerke an Flüssen geplant. Deren Kühlsysteme müssen entsprechend ausgewählt und konstruiert werden, um der zu erwartenden Erhöhung der Flusstemperaturen Rechnung zu tragen. N2 - The research described in this thesis identified a subset of German power plants that suffered from power generation reductions (WT-GR) due to high water temperature (WT) of the rivers along which they lie and due to statutory thresholds concerning mixed WT after waste heat discharge. An analysis of the recent WT and a prediction of those temperatures due to global warming were conducted. Power plants with WT-GR were identified based on a through literature search, scan of press releases and surveys. Most of WT-GR in the years between 1976 and 2007 occured in a) power plants with a gross power output of larger than 300 MW b) black coal and nuclear power plants c) power plants with once-through cooling system and d) power plants, which started operation between 1960 and 1990. Trend analysis of interpolated and harmonised recent WT of German rivers shows rising trends, predominantly in the spring and summer. Statistical analysis on numbers indicates most of days per year with either ‘very high’ or ‘extremely high’ WT in the years 1994, 2003 and 2006 in the summer. Those years also represent 63 % of all identified WT-GR, mostly between the months of June and August. The simulation of future WT considered three scenarios (named B1, A1B and A2) and three different time periods (TP) (2011-2040, 2011/2041-2070 and 2011/2071-2100). The trend analysis for 2011-2040 shows an increase in WT of the A1B and A2 scenario for at least one summer month and negative or no trends for the B1 scenario. Positive differences exist between mean WT of all three scenarios for TP 2011-2040 and mean WT of climate normal period (CNP) for at least one summer month. Estimates for the TP 2011/2041-2070 and 2011/2071-2100 and the three scenarios also show rising trends and an increase in mean WT in comparison to the CNP. Integration of above mentioned analyses indicates that plants along the rivers Isar, Rhine, Neckar, Saar, Elbe and Weser suffered most of WT-GR. Positive trends were identified by analyzing recent WT as well as the predictive WT for the period 2011-2040 and the scenarios A1B and A2 for at least one summer month. The average lifetime of a conventional thermal power plant in Germany is between 40 and 50 years. Hence it can be assumed that between 48-64 % and 67-91 %, respectively, of the power plants with an identified WT-GR will be decommissioned before 2022 and 2034, respectively, depending on the nuclear phaseout. In the case of hot summers further power generation reductions can be expected. The implication for new German power plants along rivers is that the selection, design and sizing of cooling systems must consider a further increase in river temperatures. T3 - Würzburger Geographische Arbeiten - 106 KW - Deutschland KW - Wärmekraftwerk KW - Fluss KW - Wassertemperatur KW - Klimaänderung KW - Germany KW - power plant KW - river KW - water temperature KW - global warming Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-231015 ER - TY - JOUR A1 - Alavipanah, Sadroddin A1 - Wegmann, Martin A1 - Qureshi, Salman A1 - Weng, Qihao A1 - Koellner, Thomas T1 - The role of vegetation in mitigating urban land surface temperatures: a case study of Munich, Germany during the warm season JF - Sustainability N2 - The Urban Heat Island (UHI) is the phenomenon of altered increased temperatures in urban areas compared to their rural surroundings. UHIs grow and intensify under extreme hot periods, such as during heat waves, which can affect human health and also increase the demand for energy for cooling. This study applies remote sensing and land use/land cover (LULC) data to assess the cooling effect of varying urban vegetation cover, especially during extreme warm periods, in the city of Munich, Germany. To compute the relationship between Land Surface Temperature (LST) and Land Use Land Cover (LULC), MODIS eight-day interval LST data for the months of June, July and August from 2002 to 2012 and the Corine Land Cover (CLC) database were used. Due to similarities in the behavior of surface temperature of different CLCs, some classes were reclassified and combined to form two major, rather simplified, homogenized classes: one of built-up area and one of urban vegetation. The homogenized map was merged with the MODIS eight-day interval LST data to compute the relationship between them. The results revealed that (i) the cooling effect accrued from urban vegetation tended to be non-linear; and (ii) a remarkable and stronger cooling effect in terms of LST was identified in regions where the proportion of vegetation cover was between seventy and almost eighty percent per square kilometer. The results also demonstrated that LST within urban vegetation was affected by the temperature of the surrounding built-up and that during the well-known European 2003 heat wave, suburb areas were cooler from the core of the urbanized region. This study concluded that the optimum green space for obtaining the lowest temperature is a non-linear trend. This could support urban planning strategies to facilitate appropriate applications to mitigate heat-stress in urban area. KW - Surface Urban Heat Island (SUHI) KW - cities KW - buildings KW - Land Surface Temperature (LST) KW - urban vegetation KW - climate change KW - heat waves Y1 - 2015 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-143447 VL - 7 ER - TY - JOUR A1 - Lausch, Angela A1 - Borg, Erik A1 - Bumberger, Jan A1 - Dietrich, Peter A1 - Heurich, Marco A1 - Huth, Andreas A1 - Jung, András A1 - Klenke, Reinhard A1 - Knapp, Sonja A1 - Mollenhauer, Hannes A1 - Paasche, Hendrik A1 - Paulheim, Heiko A1 - Pause, Marion A1 - Schweitzer, Christian A1 - Schmulius, Christiane A1 - Settele, Josef A1 - Skidmore, Andrew K. A1 - Wegmann, Martin A1 - Zacharias, Steffen A1 - Kirsten, Toralf A1 - Schaepman, Michael E. T1 - Understanding forest health with remote sensing, part III: requirements for a scalable multi-source forest health monitoring network based on data science approaches JF - Remote Sensing N2 - Forest ecosystems fulfill a whole host of ecosystem functions that are essential for life on our planet. However, an unprecedented level of anthropogenic influences is reducing the resilience and stability of our forest ecosystems as well as their ecosystem functions. The relationships between drivers, stress, and ecosystem functions in forest ecosystems are complex, multi-faceted, and often non-linear, and yet forest managers, decision makers, and politicians need to be able to make rapid decisions that are data-driven and based on short and long-term monitoring information, complex modeling, and analysis approaches. A huge number of long-standing and standardized forest health inventory approaches already exist, and are increasingly integrating remote-sensing based monitoring approaches. Unfortunately, these approaches in monitoring, data storage, analysis, prognosis, and assessment still do not satisfy the future requirements of information and digital knowledge processing of the 21st century. Therefore, this paper discusses and presents in detail five sets of requirements, including their relevance, necessity, and the possible solutions that would be necessary for establishing a feasible multi-source forest health monitoring network for the 21st century. Namely, these requirements are: (1) understanding the effects of multiple stressors on forest health; (2) using remote sensing (RS) approaches to monitor forest health; (3) coupling different monitoring approaches; (4) using data science as a bridge between complex and multidimensional big forest health (FH) data; and (5) a future multi-source forest health monitoring network. It became apparent that no existing monitoring approach, technique, model, or platform is sufficient on its own to monitor, model, forecast, or assess forest health and its resilience. In order to advance the development of a multi-source forest health monitoring network, we argue that in order to gain a better understanding of forest health in our complex world, it would be conducive to implement the concepts of data science with the components: (i) digitalization; (ii) standardization with metadata management after the FAIR (Findability, Accessibility, Interoperability, and Reusability) principles; (iii) Semantic Web; (iv) proof, trust, and uncertainties; (v) tools for data science analysis; and (vi) easy tools for scientists, data managers, and stakeholders for decision-making support. KW - forest health KW - in situ forest monitoring KW - remote sensing KW - data science KW - digitalization KW - big data KW - semantic web KW - linked open data KW - FAIR KW - multi-source forest health monitoring network Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-197691 SN - 2072-4292 VL - 10 IS - 7 ER - TY - JOUR A1 - Fa, John E. A1 - Olivero, Jesús A1 - Real, Raimundo A1 - Farfán, Miguel A. A1 - Márquez, Ana L. A1 - Vargas, J. Mario A1 - Ziegler, Stefan A1 - Wegmann, Martin A1 - Brown, David A1 - Margetts, Barrie A1 - Nasi, Robert T1 - Disentangling the relative effects of bushmeat availability on human nutrition in central Africa JF - Scientific Reports N2 - We studied links between human malnutrition and wild meat availability within the Rainforest Biotic Zone in central Africa. We distinguished two distinct hunted mammalian diversity distributions, one in the rainforest areas (Deep Rainforest Diversity, DRD) containing taxa of lower hunting sustainability, the other in the northern rainforest-savanna mosaic, with species of greater hunting potential (Marginal Rainforest Diversity, MRD). Wild meat availability, assessed by standing crop mammalian biomass, was greater in MRD than in DRD areas. Predicted bushmeat extraction was also higher in MRD areas. Despite this, stunting of children, a measure of human malnutrition, was greater in MRD areas. Structural equation modeling identified that, in MRD areas, mammal diversity fell away from urban areas, but proximity to these positively influenced higher stunting incidence. In DRD areas, remoteness and distance from dense human settlements and infrastructures explained lower stunting levels. Moreover, stunting was higher away from protected areas. Our results suggest that in MRD areas, forest wildlife rational use for better human nutrition is possible. By contrast, the relatively low human populations in DRD areas currently offer abundant opportunities for the continued protection of more vulnerable mammals and allow dietary needs of local populations to be met. KW - plant species richness KW - development policy KW - Congo Basin KW - conservation KW - dependence KW - wildlife consumption KW - food security KW - forests KW - biodiversity KW - hotspots Y1 - 2015 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-144110 VL - 5 IS - 8168 ER - TY - THES A1 - Kawohl, Alexander T1 - The Petrology and Geochemistry of Igneous Dykes above the Temagami Anomaly (Ontario, Canada) and their Relationship to the 1.85 Ga Sudbury Impact T1 - Die Petrologie und Geochemie magmatischer Gänge über der Temagami Anomaly (Ontario, Kanada) und ihre Beziehung zum 1,85 Ga Sudbury Impakt N2 - The area northeast of Sudbury, Ontario, is known for one of the largest unexplained geophysical anomalies on the Canadian Shield, the 1,200 km2 Temagami Anomaly. The geological cause of this regional magnetic, conductive and gravity feature has previously been modelled to be a mafic-ultramafic body at relatively great depth (2–15 km) of unknown age and origin, which may or may not be related to the meteorite impact-generated Sudbury Igneous Complex in its immediate vicinity. However, with a profound lack of outcrops and drill holes, the geological cause of the anomaly remains elusive, a genetic link to the 1.85 Ga Sudbury impact event purely speculative. In search for any potential surface expression of the deep-seated cause of the Temagami Anomaly, this study provides a first, yet comprehensive petrological and geochemical assessment of exotic igneous dykes recently discovered in outcrops above, and drill cores into, the Temagami Anomaly. Based on cross-cutting field relations, petrographic studies, lithogeochemistry, whole-rock Nd-Sr-Pb isotope systematics, and U-Pb geochronology, it was possible to identify, and distinguish between, at least six different groups of igneous dykes: (i) Calc-alkaline quartz diorite dykes related to the 1.85 Ga Sudbury Igneous Complex (locally termed Offset Dykes); (ii) tholeiitic quartz diabase of the regional 2.22 Ga Nipissing Suite/Senneterre Dyke Swarm; (iii) calc-alkaline quartz diabase of the regional 2.17 Ga Biscotasing Dyke Swarm; (iv) alkaline ultrabasic dykes correlated with the 1.88–1.86 Ga Circum-Superior Large Igneous Province (LIP); and (v) aplitic dykes as well as (vi) a hornblende syenite, the latter two of more ambiguous age and stratigraphic position. The findings presented in this study – the discovery of three new Offset Dykes in particular – offer some unexpected insights into the geology and economic potential of one of the least explored areas of the world-class Sudbury Mining Camp as well as into the nature and distribution of both allochthonous and autochthonous impactites within one of the oldest and largest impact structures known on Earth. Not only do the geometric patterns of dyke (and breccia) distribution reaffirm previous notions of the existence of discrete ring structures in the sense of a ~200-km multi-ring basin, but they provide critical constraints as to the pre-erosional thickness and extent of the impact melt sheet, thus helping to identity new areas for Ni-Cu-PGE exploration. Furthermore, this study provides important insights into the pre-impact stratigraphy and the magmatic evolution of the region in general, which reveals to be much more complex, compositionally divers, and protracted than initially assumed. Of note is the discovery of rocks related to the 2.17 Ga Biscotasing and the 1.88–1.86 Ga Circum-Superior magmatic events, as these were not previously known to occur on the southeast margin of the Superior Craton. Shortly predating the Sudbury impact and being contemporaneous with ore-forming events at Thompson (Manitoba) and Raglan (Cape Smith), these magmatic rocks could provide the missing link between unusual mafic, pre-enriched, crustal target rocks, and the unique metal endowment of the Sudbury Impact Structure. The actual geological cause of the Temagami Anomaly remains open to debate and requires the downward extension of existing bore holes as well as more detailed geophysical investigations. The hypothesis of a genetic relationship between Sudbury impact event and Temagami Anomaly is neither borne out by any evidence nor particularly realistic, even in case of an oblique impact, and should thus be abandoned. It is instead proposed, based on circumstantial evidence, that the anomaly might be explained by an ultramafic complex of the 1.88–1.86 Ga Circum-Superior LIP. N2 - Das Gebiet nordöstlich von Sudbury, Ontario, ist bekannt für eine der größten unerklärten geophysikalischen Anomalien auf dem Kanadischen Schild, die 1.200 km2 große Temagami Anomalie. Die geologische Ursache dieser regionalen magnetischen, konduktiven und Schwere-Anomalie wurde bisweilen als ein mafisch-ultramafischer Körper in relativ großer Tiefe (2–15 km) unbekannten Alters und Ursprungs modelliert, der womöglich mit dem durch einen Impakt entstandenen Sudbury Igneous Complex in dessen unmittelbarer Nachbarschaft verwandt sein könnte. Da es jedoch an Aufschlüssen und Tiefbohrungen grundlegend mangelt, bleibt die geologische Ursache dieser Anomalie unklar, eine genetische Beziehung zum 1,85 Ga Sudbury Impaktereignis rein spekulativ. Auf der Suche nach einer potenziellen Oberflächenmanifestation der tiefliegenden Ursache der Temagami Anomalie liefert diese Studie eine erste und dennoch umfassende petrologische und geochemische Charakterisierung magmatischer Ganggesteine, die erst kürzlich in Aufschlüssen über der Temagami Anomalie, als auch in Bohrkernen, entdeckt wurden. Auf Grundlage von relativen geologischen Altersbeziehungen, petrographischen Untersuchungen, Lithogeochemie, Nd-Sr-Pb Isotopensystematiken sowie U-Pb Geochronologie war es möglich, mindestens sechs Gruppen von magmatischen Gesteinsgängen zu identifizieren und zu unterscheiden: (i) kalk-alkaline Quarz Diorit Gänge, die mit dem 1,85 Ga Sudbury Igneous Complex genetisch verwandt sind (lokal als Offset Dykes bezeichnet); (ii) tholeiitischer Quarz Dolerit der regionalen 2,22 Ga Nipissing Suite/Senneterre Gangschar (iii) kalk-alkaliner Quarz Dolerit der regionalen 2,17 Ga Biscotasing Gangschar; (iv) alkaline ultrabasische Gänge, die sich mit der 1,88–1,86 Ga Circum-Superior Large Igneous Province (LIP) korrelieren lassen; und (v) aplitische Gänge sowie ein (vi) Hornblende Syenit, beide von nach wie vor unklarem Alter und unklarer Zugehörigkeit. Die in dieser Studie vorgestellten Ergebnisse – insbesondere die Entdeckung drei neuer Offset Dykes – bieten einige unerwartete Einblicke in die Geologie und das wirtschaftliche Potenzial eines der am wenigsten erforschten Gebiete des Sudbury Bergbaudistriktes sowie in die Beschaffenheit und Verteilung sowohl allochthoner als auch autochthoner Impaktgesteine innerhalb einer der größten und ältesten bekannten terrestrischen Impaktstrukturen. Die geometrischen Muster der Gang (und Brekzien-) Verteilung bestätigen nicht nur frühere Vorstellungen von der Existenz diskreter Ringstrukturen im Sinne eines ~200 km großen Multiringbeckens, sondern liefern auch Erkenntnisse über die ursprüngliche Mächtigkeit und Ausbreitung der Impaktschmelze, was unter anderem zur Identifizierung neuer potenzieller Gebiete für die Ni-Cu-PGE Exploration beiträgt. Darüber hinaus liefert diese Studie wichtige Einblicke in die Stratigraphie des Einschlagsgebietes und die magmatische Entwicklung der Region im Allgemeinen, welche sich als viel komplexer, in der Zusammensetzung vielfältiger, und zeitlich ausgedehnter erweist als ursprünglich angenommen. Hervorzuheben ist hierbei die Entdeckung von Gesteinen, die mit dem 2,17 Ga Biscotasing und dem 1,88–1,86 Circum-Superior Magmatismus in Verbindung stehen, da solche Gesteine bisher nicht am südöstlichen Rand des Superior Kratons bekannt waren. Diese Ereignisse, die kurz vor dem Sudbury Impakt und zeitgleich mit Erz-bildendem Magmatismus nahe Thompson (Manitoba) und Raglan (Cape Smith, Quebec) stattfanden, könnten das fehlende Bindeglied zwischen ungewöhnlich mafischen, vorangereicherten krustalen Zielgesteinen einerseits, und der einzigartigen Metallausstattung der Sudbury Impaktstruktur andererseits, darstellen. Die tatsächliche geologische Ursache der Temagami Anomalie bleibt nach wie vor ungeklärt und erfordert letztlich die Erweiterung bestehender Bohrlöcher sowie detailliertere geophysikalische Untersuchungen. Die Hypothese eines genetischen Zusammenhangs zwischen Sudbury Impakt und Temagami Anomalie kann weder durch Beweise gestützt werden noch gilt sie als besonders realistisch, selbst im Falle eines obliquen Einschlags, und sollte daher verworfen werden. Stattdessen wird auf der Grundlage von Indizienbeweisen vorgeschlagen, dass die Temagami Anomalie durch einen ultramafischen Komplex der 1,88–1,86 Ga Circum-Superior LIP verursacht wird. KW - Impaktstruktur KW - Magmatismus KW - Altproterozoikum KW - Lake Timagami KW - Greater Sudbury KW - Palaeoproterozoic KW - Southern Province KW - Huronian Basin KW - Sudbury Igneous Complex KW - Offset Dykes KW - Impact melts KW - Geophysical anomaly KW - PGE-Cu-Ni KW - District of Sudbury Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-279617 ER - TY - BOOK A1 - Fülling, Julia T1 - Wonach schmeckt Herkunft? – Über (Nicht-)Wissen beim Lebensmittelkonsum und die Bedeutung der Geographien und Biographien von frischem Obst und Gemüse N2 - Durch die globale Organisation von Lebensmittelwarenketten steht Konsument*innen heute ein vielfältiges, ganzjährig nahezu gleichbleibendes Angebot an frischem Obst und Gemüse im Lebensmitteleinzelhandel zur Verfügung. Damit einher geht eine erhöhte Komplexität beim Lebensmitteleinkauf und ein verändertes Wissen von Konsument*innen, über die Waren: Das eigene Erfahren der Lebensmittelproduktion ist im Alltag heute nicht mehr möglich. Statt praktischem Wissen gewinnt damit explizites und objektiviertes Wissen über die Waren, z.B. in Form von Siegeln an Bedeutung. Viele Produkt- und Produktionseigenschaften entziehen sich zudem der Kenntnis der Konsument*innen, während gleichzeitig das Bewusstsein für Fragen sozialer und ökologischer Nachhaltigkeit steigt. Die vorliegende Studie geht vor diesem Hintergrund am Beispiel des Einkaufs von frischem Obst und Gemüse der Frage nach, welche Bedeutung die Herkunftsangabe als Hinweis auf die Geographien der Waren für die Bewertung von frischem Obst und Gemüse hat und welches Wissen Konsument*innen über Waren und deren Biographien haben. Es wird zudem aufgezeigt, welche Rolle Nichtwissen beim Lebensmittelkonsum spielt. Die Studie liefert Erkenntnisse für die bislang im deutschsprachigen Raum noch vergleichsweise wenig repräsentierte Konsumgeographie und macht Konzepte aus der Wissens- und Organisationssoziologie für die wirtschaftsgeographische Forschung fruchtbar. Aus einer Praxisperspektive bietet sie Anschlusspunkte für Fragen des nachhaltigen Konsums sowie des Verbraucherschutzes. T3 - Geographische Handelsforschung - 33 KW - Konsum KW - Lebensmittel KW - Wissen KW - Globalisierung KW - Wertschöpfungskette KW - Nichtwissen KW - Regionalisierung KW - Verbraucherschutz KW - Nachhaltigkeit Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-268869 SN - 978-3-95826-182-2 SN - 978-3-95826-183-9 SN - 2196-5811 SN - 2626-8906 N1 - Parallel erschienen als Druckausgabe in Würzburg University Press, ISBN 978-3-95826-182-2, 31,80 EUR N1 - Dissertation, Humboldt-Universität zu Berlin, 2021 PB - Würzburg University Press CY - Würzburg ER - TY - RPRT A1 - Müller, Jörg A1 - Scherer-Lorenzen, Michael A1 - Ammer, Christian A1 - Eisenhauer, Nico A1 - Seidel, Dominik A1 - Schuldt, Bernhard A1 - Biedermann, Peter A1 - Schmitt, Thomas A1 - Künzer, Claudia A1 - Wegmann, Martin A1 - Cesarz, Simone A1 - Peters, Marcell A1 - Feldhaar, Heike A1 - Steffan-Dewenter, Ingolf A1 - Claßen, Alice A1 - Bässler, Claus A1 - von Oheimb, Goddert A1 - Fichtner, Andreas A1 - Thorn, Simon A1 - Weisser, Wolfgang T1 - BETA-FOR: Erhöhung der strukturellen Diversität zwischen Waldbeständen zur Erhöhung der Multidiversität und Multifunktionalität in Produktionswäldern. Antragstext für die DFG Forschungsgruppe FOR 5375 T1 - BETA-FOR: Enhancing the structural diversity between patches for improving multidiversity and multifunctionality in production forests. Proposal for DFG Research Unit FOR 5375 BT - β\(_4\) : Proposal for the 1st phase (2022-2026) of the DFG Research Unit FOR 5375/1 (DFG Forschergruppe FOR 5375/1 – BETA-FOR), Fabrikschleichach, October 2021 N2 - Der in jüngster Zeit beobachtete kontinuierliche Verlust der β-Diversität in Ökosystemen deutet auf homogene Gemeinschaften auf Landschaftsebene hin, was hauptsächlich auf die steigende Landnutzungsintensität zurückgeführt wird. Biologische Vielfalt ist mit zahlreichen Funktionen und der Stabilität von Ökosystemen verknüpft. Es ist daher zu erwarten, dass eine abnehmende β-Diversität auch die Multifunktionalität verringert. Wir kombinieren hier Fachwissen aus der Forstwissenschaft, der Ökologie, der Fernerkundung, der chemischen Ökologie und der Statistik in einem gemeinschaftlichen und experimentellen β-Diversitätsdesign, um einerseits die Auswirkungen der Homogenisierung zu bewerten und andererseits Konzepte zu entwickeln, um negative Auswirkungen durch Homogenisierung in Wäldern rückgängig zu machen. Konkret werden wir uns mit der Frage beschäftigen, ob die Verbesserung der strukturellen β-Komplexität (ESBC) in Wäldern durch Waldbau oder natürliche Störungen die Biodiversität und Multifunktionalität in ehemals homogenen Produktionswäldern erhöhen kann. Unser Ansatz wird mögliche Mechanismen hinter den beobachteten Homogenisierungs-Diversitäts-Beziehungen identifizieren und zeigen, wie sich diese auf die Multifunktionalität auswirken. An elf Standorten in ganz Deutschland haben wir dazu zwei Waldbestände als zwei kleine "Waldlandschaften" ausgewählt. In einem dieser beiden Bestände haben wir ESBC (Enhancement of Structural Beta Complexity)-Behandlungen durchgeführt. Im zweiten, dem Kontrollbestand, werden wir die gleich Anzahl 50x50m Parzellen ohne ESBC einrichten. Auf allen Parzellen werden wir 18 taxonomische Artengruppen aller trophischer Ebenen und 21 Ökosystemfunktionen, einschließlich der wichtigsten Funktionen in Wäldern der gemäßigten Zonen, messen. Der statistische Rahmen wird eine umfassende Analyse der Biodiversität ermöglichen, indem verschiedenen Aspekte (taxonomische, funktionelle und phylogenetische Vielfalt) auf verschiedenen Skalenebenen (α-, β-, γ-Diversität) quantifiziert werden. Um die Gesamtdiversität zu kombinieren, werden wir das Konzept der Multidiversität auf die 18 Taxa anwenden. Wir werden neue Ansätze zur Quantifizierung und Aufteilung der Multifunktionalität auf α- und β-Skalen verwenden und entwickeln. Durch die experimentelle Beschreibung des Zusammenhangs zwischen β-Diversität und Multifunktionalität in einer Reallandschaft wird unsere Forschung einen neuen Weg einschlagen. Darüber hinaus werden wir dazu beitragen, verbesserte Leitlinien für waldbauliche Konzepte und für das Management natürlicher Störungen zu entwickeln, um Homogenisierungseffekte der Vergangenheit umzukehren. N2 - The recently observed consistent loss of β-diversity across ecosystems indicates increasingly homogeneous communities in patches of landscapes, mainly caused by increasing land-use intensity. Biodiversity is related to numerous ecosystem functions and stability. Therefore, decreasing β-diversity is also expected to reduce multifunctionality. To assess the impact of homogenization and to develop guidelines to reverse its potentially negative effects, we combine expertise from forest science, ecology, remote sensing, chemical ecology and statistics in a collaborative and experimental β-diversity approach. Specifically, we will address the question whether the Enhancement of Structural Beta Complexity (ESBC) in forests by silviculture or natural disturbances will increase biodiversity and multifunctionality in formerly homogeneously structured production forests. Our approach will identify potential mechanisms behind observed homogenization-diversity-relationships and show how these translate into effects on multifunctionality. At eleven forest sites throughout Germany, we selected two districts as two types of small ‘forest landscapes’. In one of these two districts, we established ESBC treatments (nine differently treated 50x50 m patches with a focus on canopy cover and deadwood features). In the second, the control district, we will establish nine patches without ESBC. By a comprehensive sampling, we will monitor 18 taxonomic groups and measure 21 ecosystem functions, including key functions in temperate forests, on all patches. The statistical framework will allow a comprehensive biodiversity assessment by quantifying the different aspects of multitrophic biodiversity (taxonomical, functional and phylogenetic diversity) on different levels of biodiversity (α-, β-, γ-diversity). To combine overall diversity, we will apply the concept of multidiversity across the 18 taxa. We will use and develop new approaches for quantification and partitioning of multifunctionality at α- and β- scales. Overall, our study will herald a new research avenue, namely by experimentally describing the link between β-diversity and multifunctionality. Furthermore, we will help to develop guidelines for improved silvicultural concepts and concepts for management of natural disturbances in temperate forests reversing past homogenization effects. KW - Waldökosystem KW - Biodiversität KW - BETA-Multifunktionalität KW - beta-multifunctionality KW - BETA-Diversität KW - beta diversity KW - Forschungsstation Fabrikschleichach Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-290849 ER - TY - JOUR A1 - Buchelt, Sebastian A1 - Skov, Kirstine A1 - Rasmussen, Kerstin Krøier A1 - Ullmann, Tobias T1 - Sentinel-1 time series for mapping snow cover depletion and timing of snowmelt in Arctic periglacial environments: case study from Zackenberg and Kobbefjord, Greenland JF - The Cryosphere N2 - Snow cover (SC) and timing of snowmelt are key regulators of a wide range of Arctic ecosystem functions. Both are strongly influenced by the amplified Arctic warming and essential variables to understand environmental changes and their dynamics. This study evaluates the potential of Sentinel-1 (S-1) synthetic aperture radar (SAR) time series for monitoring SC depletion and snowmelt with high spatiotemporal resolution to capture their understudied small-scale heterogeneity. We use 97 dual-polarized S-1 SAR images acquired over northeastern Greenland and 94 over southwestern Greenland in the interferometric wide swath mode from the years 2017 and 2018. Comparison of S-1 intensity against SC fraction maps derived from orthorectified terrestrial time-lapse imagery indicates that SAR backscatter can increase before a decrease in SC fraction is observed. Hence, the increase in backscatter is related to changing snowpack properties during the runoff phase as well as decreasing SC fraction. We here present a novel empirical approach based on the temporal evolution of the SAR signal to identify start of runoff (SOR), end of snow cover (EOS) and SC extent for each S-1 observation date during melt using backscatter thresholds as well as the derivative. Comparison of SC with orthorectified time-lapse imagery indicates that HV polarization outperforms HH when using a global threshold. The derivative avoids manual selection of thresholds and adapts to different environmental settings and seasonal conditions. With a global configuration (threshold: 4 dB; polarization: HV) as well as with the derivative, the overall accuracy of SC maps was in all cases above 75 % and in more than half of cases above 90 %. Based on the physical principle of SAR backscatter during snowmelt, our approach is expected to work well in other low-vegetation areas and, hence, could support large-scale SC monitoring at high spatiotemporal resolution (20 m, 6 d) with high accuracy. KW - Greenland KW - Sentinel-1 (S-1) synthetic aperture radar (SAR) KW - snow cover depletion Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-300139 VL - 16 IS - 2 SP - 625 EP - 646 ER - TY - JOUR A1 - Rauch, Sebastian A1 - Arnold, Louisa A1 - Stuerner, Zelda A1 - Rauh, Juergen A1 - Rost, Michael T1 - A true choice of place of birth? Swiss women’s access to birth hospitals and birth centers JF - PLoS ONE N2 - While the place of birth plays a crucial role for women’s birth experiences, the interest in out-of-hospital births has increased during the Covid-19 pandemic. Related to this, various international policies recommend enabling women to choose where to give birth. We aimed to analyze Swiss women’s choice between birth hospitals and birth centers. Employing spatial accessibility analysis, we incorporated four data types: highly disaggregated population data, administrative data, street network data, addresses of birth hospitals and birth centers. 99.8% of Swiss women of childbearing age were included in the analysis (N = 1.896.669). We modelled car travel times from a woman’s residence to the nearest birth hospital and birth center. If both birth settings were available within 30 minutes, a woman was considered to have a true choice. Only 58.2% of women had a true choice. This proportion varied considerably across Swiss federal states. The main barrier to a true choice was limited accessibility of birth centers. Median travel time to birth hospitals was 9.8 (M = 12.5), to birth centers 23.9 minutes (M = 28.5). Swiss women are insufficiently empowered to exercise their reproductive autonomy as their choice of place of birth is significantly limited by geographical constraints. It is an ethical and medical imperative to provide women with a true choice. We provide high-resolution insights into the accessibility of birth settings and strong arguments to (re-)examine the need for further birth centers (and birth hospitals) in specific geographical areas. Policy-makers are obligated to improve the accessibility of birth centers to advance women’s autonomy and enhance maternal health outcomes after childbirth. The Covid-19 pandemic offers an opportunity to shift policy. KW - Switzerland KW - birth hospitals KW - access Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-300159 VL - 17 IS - 7 ER - TY - RPRT A1 - Meyer, Constantin A1 - Job, Hubert A1 - Laner, Peter A1 - Omizzolo, Andrea A1 - Kollmann, Nadia A1 - Clare, Jasmin A1 - Vesely, Philipp A1 - Riedler, Walter A1 - Plassmann, Guido A1 - Coronado, Oriana A1 - Praper Gulič, Sergeja A1 - Gulič, Andrej A1 - Koblar, Simon A1 - Teofili, Corrado A1 - Rohringer, Verena A1 - Schoßleitner, Richard A1 - Ainz, Gerhard T1 - OpenSpaceAlps Planungshandbuch: Perspektiven für eine konsistente Freiraumsicherung im Alpenraum T1 - OpenSpaceAlps Planning Handbook: Perspectives for consistent safeguarding of open spaces in the Alpine region N2 - Im Alpenraum lässt sich nach wie vor die kontinuierliche Inanspruchnahme von Freiräumen für Siedlungsflächen und technische Infrastrukturen und die damit verbundene Bodenversiegelung beobachten. Dies führt in erster Linie zum Verlust von landwirtschaftlichen Flächen. Je nach Ausmaß der Bebauung kommt es auch zu einer verstärkten Landschaftszerschneidung, die zur Isolierung natürlicher Lebensräume und zur Einschränkung des ökologischen Verbundes sowie zu weiteren negativen Folgewirkungen führt. Das OpenSpaceAlps Projekt hat sich dieser Thematik angenommen und, basierend auf kooperativen Verfahren in mehreren Pilotregionen, Handlungsansätze und Strategien für eine nachhaltige Sicherung von Freiräumen entwickelt. Dieses Handbuch stellt eine Handlungs- und Entscheidungshilfe für verschiedene Akteure/Akteurinnen dar, allen voran Planer*innen in öffentlichen Planungsbehörden. Ausgehend von einer Analyse der Herausforderungen und Rahmenbedingungen im Alpenraum, werden in diesem Handbuch zentrale „Prinzipien“ der Freiraumplanung vorgestellt und verglichen. Außerdem werden integrierte Planungsstrategien für verschiedene Raumkategorien diskutiert. KW - Raumordnung KW - Alpen KW - Alpen KW - OpenSpaceAlps KW - Freiraum KW - Raumplanung KW - Transnationale Zusammenarbeit Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-273070 N1 - English version available at: https://doi.org/10.25972/OPUS-27040. Italian version available at: https://doi.org/10.25972/OPUS-27704. N1 - The OpenSpaceAlps project is co-financed by the European Regional Development Fund through the Interreg Alpine Space programme. ER - TY - THES A1 - Wilde, Martina T1 - Landslide susceptibility assessment in the Chiconquiaco Mountain Range area, Veracruz (Mexico) T1 - Bewertung der Rutschungssuszeptibilität in der Chiconquiaco Gebirgsregion, Veracruz (Mexiko) N2 - In Mexico, numerous landslides occur each year and Veracruz represents the state with the third highest number of events. Especially the Chiconquiaco Mountain Range, located in the central part of Veracruz, is highly affected by landslides and no detailed information on the spatial distribution of existing landslides or future occurrences is available. This leaves the local population exposed to an unknown threat and unable to react appropriately to this hazard or to consider the potential landslide occurrence in future planning processes. Thus, the overall objective of the present study is to provide a comprehensive assessment of the landslide situation in the Chiconquiaco Mountain Range area. Here, the combination of a site-specific and a regional approach enables to investigate the causes, triggers, and process types as well as to model the landslide susceptibility for the entire study area. For the site-specific approach, the focus lies on characterizing the Capulín landslide, which represents one of the largest mass movements in the area. In this context, the task is to develop a multi-methodological concept, which concentrates on cost-effective, flexible and non-invasive methods. This approach shows that the applied methods complement each other very well and their combination allows for a detailed characterization of the landslide. The analyses revealed that the Capulín landslide is a complex mass movement type. It comprises rotational movement in the upper parts and translational movement in the lower areas, as well as flow processes at the flank and foot area and therefore, is classified as a compound slide-flow according to Cruden and Varnes (1996). Furthermore, the investigations show that the Capulín landslide represents a reactivation of a former process. This is an important new information, especially with regard to the other landslides identified in the study area. Both the road reconstructed after the landslide, which runs through the landslide mass, and the stream causing erosion processes at the foot of the landslide severely affect the stability of the landslide, making it highly susceptible to future reactivation processes. This is particularly important as the landslide is located only few hundred meters from the village El Capulín and an extension of the landslide area could cause severe damage. The next step in the landslide assessment consists of integrating the data obtained in the site-specific approach into the regional analysis. Here, the focus lies on transferring the generated data to the entire study area. The developed methodological concept yields applicable results, which is supported by different validation approaches. The susceptibility modeling as well as the landslide inventory reveal that the highest probability of landslides occurrence is related to the areas with moderate slopes covered by slope deposits. These slope deposits comprise material from old mass movements and erosion processes and are highly susceptible to landslides. The results give new insights into the landslide situation in the Chiconquiaco Mountain Range area, since previously landslide occurrence was related to steep slopes of basalt and andesite. The susceptibility map is a contribution to a better assessment of the landslide situation in the study area and simultaneously proves that it is crucial to include specific characteristics of the respective area into the modeling process, otherwise it is possible that the local conditions will not be represented correctly. N2 - In Mexico ereignen sich jedes Jahr zahlreiche Rutschungen und Veracruz ist der Bundesstaat mit der dritthöchsten Anzahl von solchen Ereignissen. Besonders das Chiconquiaco Gebirge, welches im zentralen Bereich von Veracruz liegt, ist stark von Rutschungen betroffen und trotzdem sind keine detaillierten Informationen zur räumlichen Verbreitung existierender Rutschungen oder zu deren erwarteten, zukünftigen Auftreten verfügbar. Dadurch ist die lokale Bevölkerung mit einer nicht einschätzbaren Bedrohungslage konfrontiert und kann weder auf diese angemessen reagieren noch das potentielle Auftreten von Rutschungen in künftigen Planungsprozessen berücksichtigen. Das übergeordnete Ziel der vorliegenden Arbeit besteht daher darin, eine umfassende Beurteilung der Rutschungssituation im Chiconquiaco Gebirge zu erstellen. Hierbei ermöglicht die Kombination eines standortspezifischen und eines regionalen Ansatzes sowohl die Untersuchung der Ursachen, Auslöser und Prozesstypen, als auch die Modellierung der Rutschanfälligkeit für das gesamte Untersuchungsgebiet. Bei dem standortspezifischen Ansatz liegt der Schwerpunkt auf der Charakterisierung der Capulín Rutschung, bei der es sich um eine der größten Massenbewegungen in dieser Region handelt. In diesem Rahmen besteht die Aufgabe darin, ein multi-methodologisches Konzept zu entwickeln, welches sich hauptsächlich auf kostengünstige, flexible und nicht-invasive Methoden konzentriert. Dieser Ansatz zeigt, dass sich die verwendeten Methoden sehr gut ergänzen und ihre Kombination eine detaillierte Charakterisierung der Rutschung ermöglicht. Die Ergebnisse legen dar, dass die Capulín Rutschung eine komplexe Massenbewegung ist. So umfasst sie Rotationsbewegungen im oberen und Translationsbewegungen im unteren Bereich, sowie Fließprozesse an der Flanke und im Fußbereich und kann daher nach Cruden und Varnes (1996) als Kombination aus Gleit- und Fließprozessen (compound slide-flow) klassifiziert werden. Des Weiteren zeigen die Ergebnisse, dass es sich bei der Capulín Rutschung um eine Reaktivierung einer älteren Rutschung handelt. Das ist eine wichtige neue Erkenntnis besonders im Hinblick auf die anderen Rutschungen, die im Untersuchungsgebiet festgestellt wurden. Sowohl die nach der Rutschung wieder aufgebaute Straße, die durch die Rutschmasse verläuft, als auch der Fluss, der Erosionsprozesse am Fuß der Rutschung verursacht, beeinträchtigen die Stabilität der Capulín Rutschung maßgeblich, was sie sehr anfällig für zukünftige Reaktivierungsprozesse macht. Dies ist besonders wichtig, da die Rutschung nur wenige hundert Meter von dem Ort El Capulín entfernt ist und eine Erweiterung des Rutschgebietes erhebliche Schäden verursachen könnte. Im Anschluss werden die durch den lokalen Ansatz erhaltenen Daten in die regionale Analyse integriert. Der Fokus bei diesem Vorgehen liegt dabei auf der Übertragung der generierten Daten auf das gesamte Untersuchungsgebiet. Das hier entwickelte methodische Konzept erzielt verwertbare Ergebnisse, was durch verschiedene Validierungsansätze bekräftigt werden kann. Sowohl die Suszeptibilitätsmodellierung als auch das Rutschungsinventar zeigen, dass die höchste Wahrscheinlichkeit für das Auftreten von Rutschungen vor allem in den Gebieten mit moderater Hangneigung liegt, welche mit Hangschutt bedeckt sind. Diese Hangablagerungen bestehen aus Material von alten Massenbewegungen und Erosionsprozessen und zeigen eine hohe Anfälligkeit für Rutschungen. Die Ergebnisse liefern neue Erkenntnisse über die Rutschungssituation im Chiconquiaco Gebirge, da vorher das Auftreten von Rutschungen mit den steilen Hängen aus Basalt und Andesit in Verbindung gebracht wurde. Auf Grundlage der generierten Suszeptibilitätskarte ist eine bessere Bewertung der Rutschungssituation im Untersuchungsgebiet möglich. Weiterhin zeigt sie, dass es von entscheidender Bedeutung ist, spezifische Eigenschaften der jeweiligen Untersuchungsgebiete in die Modellierung miteinzubeziehen, da sonst die Gefahr besteht, dass die örtlichen Gegebenheiten fehlerhaft eingeschätzt werden. KW - Naturgefahren KW - Landslide susceptibility modeling KW - Geomorphologie KW - Rutschungen KW - Modellierung KW - Veracruz KW - Mexiko KW - UAV KW - Digital Elevation Model KW - Hangstabilitätsmodellierung Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-276085 ER - TY - THES A1 - Ibebuchi, Chibuike Chiedozie T1 - Bias correction of climate model output for Germany T1 - Bias-Korrektur des Klimamodell-Outputs für Deutschland N2 - Regional climate models (RCMs) are tools used to project future climate change at a regional scale. Despite their high horizontal resolution, RCMs are characterized by systematic biases relative to observations, which can result in unrealistic interpretations of future climate change signals. On the other hand, bias correction (BC) is a popular statistical post-processing technique applied to improve the usability of output from climate models. Like every other statistical technique, BC has its strengths and weaknesses. Hence, within the regional context of Germany, and for temperature and precipitation, this study is dedicated to the assessment of the impact of different BC techniques on the RCM output. The focuses are on the impact of BC on the RCM’s statistical characterization, and physical consistency defined as the spatiotemporal consistency between the bias-corrected variable and the simulated physical mechanisms governing the variable, as well as the correlations between the bias-corrected variable and other (simulated) climate variables. Five BC techniques were applied in adjusting the systematic biases in temperature and precipitation RCM outputs. The BC techniques are linear scaling, empirical quantile mapping, univariate quantile delta mapping, multivariate quantile delta mapping that considers inter-site dependencies, and multivariate quantile delta mapping that considers inter-variable dependencies (MBCn). The results show that each BC technique adds value in reducing the biases in the statistics of the RCM output, though the added value depends on several factors such as the temporal resolution of the data, choice of RCM, climate variable, region, and the metric used in evaluating the BC technique. Further, the raw RCMs reproduced portions of the observed modes of atmospheric circulation in Western Europe, and the observed temperature, and precipitation meteorological patterns in Germany. After the BC, generally, the spatiotemporal configurations of the simulated meteorological patterns as well as the governing large-scale mechanisms were reproduced. However, at a more localized spatial scale for the individual meteorological patterns, the BC changed the simulated co-variability of some grids, especially for precipitation. Concerning the co-variability among the variables, a physically interpretable positive correlation was found between temperature and precipitation during boreal winter in both models and observations. For most grid boxes in the study domain and on average, the BC techniques that do not adjust inter-variable dependency did not notably change the simulated correlations between the climate variables. However, depending on the grid box, the (univariate) BC techniques tend to degrade the simulated temporal correlations between temperature and precipitation. Further, MBCn which adjusts biases in inter-variable dependency has the skill to improve the correlations between the simulated variables towards observations. N2 - Regionale Klimamodelle (RCMs) sind Werkzeuge, die verwendet werden, um den zukünftigen Klimawandel auf regionaler Ebene zu prognostizieren. Trotz ihrer hohen horizontalen Auflösung sind RCMs je nach Beobachtung durch systematische Verzerrungen gekennzeichnet, was zu unrealistischen Interpretationen zukünftiger Signale des Klimawandels führen kann. Andererseits ist die Bias-Korrektur (BC) eine beliebte statistische Nachbearbeitungstechnik, die angewendet wird, um die Nutzbarkeit der Ergebnisse von Klimamodellen zu verbessern. Wie jede andere statistische Technik hat BC seine Stärken und Schwächen. Daher widmet sich diese Studie im regionalen Kontext Deutschlands und für Temperatur und Niederschlag der Bewertung der Auswirkungen verschiedener BC-Techniken auf den das RCM-ErtragErgebnis. Die Schwerpunkte liegen auf der Auswirkung von BC auf die statistische Charakterisierung des RCM und auf der physikalischen Konsistenz. Letztere ist, definiert als die räumlich-zeitliche Konsistenz zwischen der systematisch korrigierten Variablen und den simulierten physikalischen Mechanismen, die diese Variable steuern, sowie auf den Korrelationen zwischen der systematisch korrigierten Variablen und anderen (simulierten) Klimavariablen. Fünf BC-Techniken wurden angewendet, um die systematischen Abweichungen in den Temperatur- und Niederschlags-RCM-Ausgaben Ergebnissen anzupassen. Die BC-Techniken sind lineare Skalierung, empirisches Quantil-Mapping, univariates Quantil-Delta-Mapping, sowie multivariates Quantil-Delta-Mapping, das Abhängigkeiten zwischen Standorten berücksichtigt, und multivariates Quantil-Delta-Mapping, das intervariable Abhängigkeiten (MBCn) berücksichtigt. Die Ergebnisse zeigen, dass jede BC-Technik einen Mehrwert bei der Reduzierung der Verzerrungen in den Statistiken der RCM-Ausgabe bringt, und dies, obwohl der Mehrwert von mehreren Faktoren abhängt, wie der zeitlichen Auflösung der Daten, der Wahl der RCM, der Klimavariable, der Region und desr verwendeten Massstabsetrik zur Bewertung der BC-Technik verwendet. Darüber hinaus reproduzierten die rohen RCMs Teile der beobachteten Modi der atmosphärischen Zirkulation in Westeuropa und die beobachteten meteorologischen Temperatur- und Niederschlagsmuster in Deutschland. Nach der BC wurden im Allgemeinen die raumzeitlichen Konfigurationen der simulierten meteorologischen Muster sowie die maßgeblichen großräumigen Mechanismen reproduziert. Auf einer stärker lokalisierten räumlichen Skala änderte der BC jedoch für die einzelnen meteorologischen Muster die simulierte Kovariabilität einiger Gitter, insbesondere für Niederschlag. Bezüglich der Kovariabilität zwischen den Variablen wurde sowohl in Modellen als auch in Beobachtungen eine physikalisch interpretierbare positive Korrelation zwischen Temperatur und Niederschlag im borealen Winter gefunden. Für die meisten Gitterboxen Gitterfelder im Untersuchungsbereich und auch im Durchschnitt änderten die BC-Techniken, die die Abhängigkeit zwischen den Variablen nicht anpassen, die simulierten Korrelationen zwischen den Klimavariablen nicht merklich. Allerdings neigen die (univariaten) BC-Techniken je nach Gitterbox Gitterfeld dazu, die simulierten zeitlichen Korrelationen zwischen Temperatur und Niederschlag zu verschlechtern. Darüber hinaus hat MBCn, das Verzerrungen in der Abhängigkeit zwischen Variablen anpasst, die Fähigkeit, die Korrelationen zwischen den simulierten Variablen gegenüber den Beobachtungen zu verbessern. KW - Bias correction KW - regional climate models KW - Germany KW - physical consistency KW - meteorological patterns KW - Bias-Korrektur KW - Regionale Klimamodelle KW - Deutschland KW - Physikalische Konsistenz KW - Meteorologische Muster Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-312647 ER - TY - JOUR A1 - Ibebuchi, Chibuike Chiedozie A1 - Schönbein, Daniel A1 - Adakudlu, Muralidhar A1 - Xoplaki, Elena A1 - Paeth, Heiko T1 - Comparison of three techniques to adjust daily precipitation biases from regional climate models over Germany JF - Water N2 - This study compares the performance of three bias correction (BC) techniques in adjusting simulated precipitation estimates over Germany. The BC techniques are the multivariate quantile delta mapping (MQDM) where the grids are used as variables to incorporate the spatial dependency structure of precipitation in the bias correction; empirical quantile mapping (EQM) and, the linear scaling (LS) approach. Several metrics that include first to fourth moments and extremes characterized by the frequency of heavy wet days and return periods during boreal summer were applied to score the performance of the BC techniques. Our results indicate a strong dependency of the relative performances of the BC techniques on the choice of the regional climate model (RCM), the region, the season, and the metrics of interest. Hence, each BC technique has relative strengths and weaknesses. The LS approach performs well in adjusting the first moment but tends to fall short for higher moments and extreme precipitation during boreal summer. Depending on the season, the region and the RCM considered, there is a trade-off between the relative performances of the EQM and the MQDM in adjusting the simulated precipitation biases. However, the MQDM performs well across all considered metrics. Overall, the MQDM outperforms the EQM in improving the higher moments and in capturing the observed return level of extreme summer precipitation, averaged over Germany. KW - bias correction KW - multivariate quantile delta mapping KW - empirical quantile mapping KW - linear scaling KW - precipitation KW - Germany Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-262064 SN - 2073-4441 VL - 14 IS - 4 ER - TY - JOUR A1 - Nyamekye, Clement A1 - Thiel, Michael A1 - Schönbrodt-Stitt, Sarah A1 - Zoungrana, Benewinde J.-B. A1 - Amekudzi, Leonard K. T1 - Soil and water conservation in Burkina Faso, West Africa JF - Sustainability N2 - Inadequate land management and agricultural activities have largely resulted in land degradation in Burkina Faso. The nationwide governmental and institutional driven implementation and adoption of soil and water conservation measures (SWCM) since the early 1960s, however, is expected to successively slow down the degradation process and to increase the agricultural output. Even though relevant measures have been taken, only a few studies have been conducted to quantify their effect, for instance, on soil erosion and environmental restoration. In addition, a comprehensive summary of initiatives, implementation strategies, and eventually region-specific requirements for adopting different SWCM is missing. The present study therefore aims to review the different SWCM in Burkina Faso and implementation programs, as well as to provide information on their effects on environmental restoration and agricultural productivity. This was achieved by considering over 143 studies focusing on Burkina Faso’s experience and research progress in areas of SWCM and soil erosion. SWCM in Burkina Faso have largely resulted in an increase in agricultural productivity and improvement in food security. Finally, this study aims at supporting the country’s informed decision-making for extending already existing SWCM and for deriving further implementation strategies. KW - soil and water conservation KW - environmental degradation KW - agricultural productivity KW - food security KW - soil erosion KW - Burkina Faso Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-197653 SN - 2071-1050 VL - 10 IS - 9 ER - TY - JOUR A1 - Steininger, Michael A1 - Abel, Daniel A1 - Ziegler, Katrin A1 - Krause, Anna A1 - Paeth, Heiko A1 - Hotho, Andreas T1 - ConvMOS: climate model output statistics with deep learning JF - Data Mining and Knowledge Discovery N2 - Climate models are the tool of choice for scientists researching climate change. Like all models they suffer from errors, particularly systematic and location-specific representation errors. One way to reduce these errors is model output statistics (MOS) where the model output is fitted to observational data with machine learning. In this work, we assess the use of convolutional Deep Learning climate MOS approaches and present the ConvMOS architecture which is specifically designed based on the observation that there are systematic and location-specific errors in the precipitation estimates of climate models. We apply ConvMOS models to the simulated precipitation of the regional climate model REMO, showing that a combination of per-location model parameters for reducing location-specific errors and global model parameters for reducing systematic errors is indeed beneficial for MOS performance. We find that ConvMOS models can reduce errors considerably and perform significantly better than three commonly used MOS approaches and plain ResNet and U-Net models in most cases. Our results show that non-linear MOS models underestimate the number of extreme precipitation events, which we alleviate by training models specialized towards extreme precipitation events with the imbalanced regression method DenseLoss. While we consider climate MOS, we argue that aspects of ConvMOS may also be beneficial in other domains with geospatial data, such as air pollution modeling or weather forecasts. KW - Klima KW - Modell KW - Deep learning KW - Neuronales Netz KW - climate KW - neural networks KW - model output statistics Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324213 SN - 1384-5810 VL - 37 IS - 1 ER - TY - JOUR A1 - Ibebuchi, Chibuike Chiedozie A1 - Schönbein, Daniel A1 - Paeth, Heiko T1 - On the added value of statistical post-processing of regional climate models to identify homogeneous patterns of summer rainfall anomalies in Germany JF - Climate Dynamics N2 - A fuzzy classification scheme that results in physically interpretable meteorological patterns associated with rainfall generation is applied to classify homogeneous regions of boreal summer rainfall anomalies in Germany. Four leading homogeneous regions are classified, representing the western, southeastern, eastern, and northern/northwestern parts of Germany with some overlap in the central parts of Germany. Variations of the sea level pressure gradient across Europe, e.g., between the continental and maritime regions, is the major phenomenon that triggers the time development of the rainfall regions by modulating wind patterns and moisture advection. Two regional climate models (REMO and CCLM4) were used to investigate the capability of climate models to reproduce the observed summer rainfall regions. Both regional climate models (RCMs) were once driven by the ERA-Interim reanalysis and once by the MPI-ESM general circulation model (GCM). Overall, the RCMs exhibit good performance in terms of the regionalization of summer rainfall in Germany; though the goodness-of-match with the rainfall regions/patterns from observational data is low in some cases and the REMO model driven by MPI-ESM fails to reproduce the western homogeneous rainfall region. Under future climate change, virtually the same leading modes of summer rainfall occur, suggesting that the basic synoptic processes associated with the regional patterns remain the same over Germany. We have also assessed the added value of bias-correcting the MPI-ESM driven RCMs using a simple linear scaling approach. The bias correction does not significantly alter the identification of homogeneous rainfall regions and, hence, does not improve their goodness-of-match compared to the observed patterns, except for the one case where the original RCM output completely fails to reproduce the observed pattern. While the linear scaling method improves the basic statistics of precipitation, it does not improve the simulated meteorological patterns represented by the precipitation regimes. KW - summer precipitation regions KW - Germany KW - climate models KW - fuzzy classification KW - bias correction Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324122 SN - 0930-7575 VL - 59 IS - 9-10 ER - TY - JOUR A1 - Geyer, Gerd A1 - Landing, Ed A1 - Meier, Stefan A1 - Höhn, Stefan T1 - Oldest known West Gondwanan graptolite: Ovetograptus? sp. (lower Agdzian/lowest Wuliuan; basal Middle Cambrian) of the Franconian Forest, Germany, and review of pre-Furongian graptolithoids JF - Paläontologische Zeitschrift N2 - The occurrence of a likely graptolite in lowest Wuliuan strata of the Franconian Forest almost certainly records the oldest known graptolithoid hemichordate in West Gondwana and possibly the oldest graptolite presently known. The fossil is a delicate, erect, apparently unbranched rhabdosome with narrow thecae tentatively assigned to the poorly known genus Ovetograptus of the Dithecodendridae. This report includes an overview of pre-Furongian graptolithoids with slight corrections on the stratigraphic position of earlier reported species. KW - Cambrian KW - Graptolithoidea KW - biostratigraphy KW - morphology KW - West Gondwana Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324099 SN - 0031-0220 VL - 97 IS - 4 ER - TY - JOUR A1 - Rai, P. A1 - Ziegler, K. A1 - Abel, D. A1 - Pollinger, F. A1 - Paeth, H. T1 - Performance of a regional climate model with interactive vegetation (REMO-iMOVE) over Central Asia JF - Theoretical and Applied Climatology N2 - The current study evaluates the regional climate model REMO (v2015) and its new version REMO-iMOVE, including interactive vegetation and plant functional types (PFTs), over two Central Asian domains for the period of 2000–2015 at two different horizontal resolutions (0.44° and 0.11°). Various statistical metrices along with mean bias patterns for precipitation, temperature, and leaf area index have been used for the model evaluation. A better representation of the spatial pattern of precipitation is found at 0.11° resolution over most of Central Asia. Regarding the mean temperature, both model versions show a high level of agreement with the validation data, especially at the higher resolution. This also reduces the biases in maximum and minimum temperature. Generally, REMO-iMOVE shows an improvement regarding the temperature bias but produces a larger precipitation bias compared to the REMO conventional version with interannually static vegetation. Since the coupled version is capable to simulate the mean climate of Central Asia like its parent version, both can be used for impact studies and future projections. However, regarding the new vegetation scheme and its spatiotemporal representation exemplified by the leaf area index, REMO-iMOVE shows a clear advantage over REMO. This better simulation is caused by the implementation of more realistic and interactive vegetation and related atmospheric processes which consequently add value to the regional climate model. KW - regional climate model (RCM) KW - interactive vegetation KW - REMO-iMOVE KW - Central Asia KW - evaluation Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324155 SN - 0177-798X VL - 150 IS - 3-4 ER - TY - JOUR A1 - Libanda, Brigadier T1 - Performance assessment of CORDEX regional climate models in wind speed simulations over Zambia JF - Modeling Earth Systems and Environment N2 - There is no single solution to cutting emissions, however, renewable energy projects that are backed by rigorous ex-ante assessments play an important role in these efforts. An inspection of literature reveals critical knowledge gaps in the understanding of future wind speed variability across Zambia, thus leading to major uncertainties in the understanding of renewable wind energy potential over the country. Several model performance metrics, both statistical and graphical were used in this study to examine the performance of CORDEX Africa Regional Climate Models (RCMs) in simulating wind speed across Zambia. Results indicate that wind speed is increasing at the rate of 0.006 m s\(^{−1}\) per year. RCA4-GFDL-ESM2M, RCA4-HadGEM2-ES, RCA4-IPSL-CM5A-MR, and RCA4-CSIRO-MK3.6.0 were found to correctly simulate wind speed increase with varying magnitudes on the Sen’s estimator of slope. All the models sufficiently reproduce the annual cycle of wind speed with a steady increase being observed from April reaching its peak around August/September and beginning to drop in October. Apart from RegCM4-MPI-ESM and RegCM4-HadGEM2, the performance of RCMs in simulating spatial wind speed patterns is generally good although they overestimate it by ~ 1 m s\(^{−1}\) in the western and southern provinces of the country. Model performance metrics indicate that with a correlation coefficient of 0.5, a root mean square error of 0.4 m s\(^{−1}\), an RSR value of 7.7 and a bias of 19.9%, RCA4-GFDL-ESM2M outperforms all other models followed by RCA4-HadGEM2, and RCA4-CM5A-MR respectively. These results, therefore, suggest that studies that use an ensemble of RCA4-GFDL-ESM2M, RCA4-HadGEM2, and RCA4-CM5A-MR would yield useful results for informing future renewable wind energy potential in Zambia. KW - renewable energy KW - wind speed KW - CORDEX Africa KW - Zambia Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324147 SN - 2363-6203 VL - 9 IS - 1 ER - TY - JOUR A1 - Kanmegne Tamga, Dan A1 - Latifi, Hooman A1 - Ullmann, Tobias A1 - Baumhauer, Roland A1 - Thiel, Michael A1 - Bayala, Jules T1 - Modelling the spatial distribution of the classification error of remote sensing data in cocoa agroforestry systems JF - Agroforestry Systems N2 - Cocoa growing is one of the main activities in humid West Africa, which is mainly grown in pure stands. It is the main driver of deforestation and encroachment in protected areas. Cocoa agroforestry systems which have been promoted to mitigate deforestation, needs to be accurately delineated to support a valid monitoring system. Therefore, the aim of this research is to model the spatial distribution of uncertainties in the classification cocoa agroforestry. The study was carried out in Côte d’Ivoire, close to the Taï National Park. The analysis followed three steps (i) image classification based on texture parameters and vegetation indices from Sentinel-1 and -2 data respectively, to train a random forest algorithm. A classified map with the associated probability maps was generated. (ii) Shannon entropy was calculated from the probability maps, to get the error maps at different thresholds (0.2, 0.3, 0.4 and 0.5). Then, (iii) the generated error maps were analysed using a Geographically Weighted Regression model to check for spatial autocorrelation. From the results, a producer accuracy (0.88) and a user’s accuracy (0.91) were obtained. A small threshold value overestimates the classification error, while a larger threshold will underestimate it. The optimal value was found to be between 0.3 and 0.4. There was no evidence of spatial autocorrelation except for a smaller threshold (0.2). The approach differentiated cocoa from other landcover and detected encroachment in forest. Even though some information was lost in the process, the method is effective for mapping cocoa plantations in Côte d’Ivoire. KW - cocoa mapping KW - geographically weighted regression KW - Sentinel-1 KW - Sentinel-2 KW - Shannon entropy KW - spatial error assessment Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324139 SN - 0167-4366 VL - 97 IS - 1 ER - TY - JOUR A1 - Frimmel, Hartwig E. A1 - Chakravarti, Rajarshi A1 - Basei, Miguel A. S. T1 - Detrital zircon ages from Archaean conglomerates in the Singhbhum Craton, eastern India: implications on economic Au-U potential JF - Mineralium Deposita N2 - New U–Pb age and Hf isotope data obtained on detrital zircon grains from Au- and U-bearing Archaean quartz-pebble conglomerates in the Singhbhum Craton, eastern India, specifically the Upper Iron Ore Group in the Badampahar Greenstone Belt and the Phuljhari Formation below the Dhanjori Group provide insights into the zircon provenance and maximum age of sediment deposition. The most concordant, least disturbed \(^{207}\)Pb/\(^{206}\)Pb ages cover the entire range of known magmatic and higher grade metamorphic events in the craton from 3.48 to 3.06 Ga and show a broad maximum between 3.38 and 3.18 Ga. This overlap is also mimicked by Lu–Hf isotope analyses, which returned a wide range in \(_{εHf}\)(t) values from + 6 to − 5, in agreement with the range known from zircon grains in igneous and metamorphic rocks in the Singhbhum Craton. A smaller but distinct age peak centred at 3.06 Ga corresponds to the age of the last major magmatic intrusive event, the emplacement of the Mayurbhanj Granite and associated gabbro, picrite and anorthosite. Thus, these intrusive rocks must form a basement rather than being intrusive into the studied conglomerates as previously interpreted. The corresponding detrital zircon grains all have a subchondritic Hf isotopic composition. The youngest reliable zircon ages of 3.03 Ga in the case of the basal Upper Iron Ore Group in the east of the craton and 3.00 Ga for the Phuljhari Formation set an upper limit on the age of conglomerate sedimentation. Previously published detrital zircon age data from similarly Au-bearing conglomerates in the Mahagiri Quartzite in the Upper Iron Ore Group in the south of the craton gave a somewhat younger maximum age of sedimentation of 2.91 Ga. There, the lower limit on sedimentation is given by an intrusive relationship with a c. 2.8 Ga granite. The time window thus defined for conglomerate deposition on the Singhbhum Craton is almost identical to the age span established for the, in places, Au- and U-rich conglomerates in the Kaapvaal Craton of South Africa: the 2.98–2.78 Ga Dominion Group and Witwatersrand Supergroup in South Africa. Since the recognition of first major concentration of gold on Earth’s surface by microbial activity having taken place at around 2.9 Ga, independent of the nature of the hinterland, the above similarity in age substantially increases the potential for discovering Witwatersrand-type gold and/or uranium deposits on the Singhbhum Craton. Further age constraints are needed there, however, to distinguish between supposedly less fertile (with respect to Au) > 2.9 Ga and more fertile < 2.9 Ga successions. KW - quartz-pebble conglomerate KW - gold KW - Mesoarchaean KW - Singhbhum Craton KW - zircon geochronology Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324084 SN - 0026-4598 VL - 57 IS - 8 ER - TY - JOUR A1 - Ibebuchi, Chibuike Chiedozie T1 - Circulation patterns linked to the positive sub-tropical Indian Ocean dipole JF - Advances in Atmospheric Sciences N2 - The positive phase of the subtropical Indian Ocean dipole (SIOD) is one of the climatic modes in the subtropical southern Indian Ocean that influences the austral summer inter-annual rainfall variability in parts of southern Africa. This paper examines austral summer rain-bearing circulation types (CTs) in Africa south of the equator that are related to the positive SIOD and the dynamics through which specific rainfall regions in southern Africa can be influenced by this relationship. Four austral summer rain-bearing CTs were obtained. Among the four CTs, the CT that featured (i) enhanced cyclonic activity in the southwest Indian Ocean; (ii) positive widespread rainfall anomaly in the southwest Indian Ocean; and (iii) low-level convergence of moisture fluxes from the tropical South Atlantic Ocean, tropical Indian Ocean, and the southwest Indian Ocean, over the south-central landmass of Africa, was found to be related to the positive SIOD climatic mode. The relationship also implies that positive SIOD can be expected to increase the amplitude and frequency of occurrence of the aforementioned CT. The linkage between the CT related to the positive SIOD and austral summer homogeneous regions of rainfall anomalies in Africa south of the equator showed that it is the principal CT that is related to the inter-annual rainfall variability of the south-central regions of Africa, where the SIOD is already known to significantly influence its rainfall variability. Hence, through the large-scale patterns of atmospheric circulation associated with the CT, the SIOD can influence the spatial distribution and intensity of rainfall over the preferred landmass through enhanced moisture convergence. KW - subtropical Indian Ocean dipole KW - circulation types KW - rainfall KW - South Indian Ocean KW - moisture convergence Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324119 SN - 0256-1530 VL - 40 IS - 1 ER - TY - JOUR A1 - Fäth, Julian A1 - Kunz, Julius A1 - Kneisel, Christof T1 - Monitoring spatiotemporal soil moisture changes in the subsurface of forest sites using electrical resistivity tomography (ERT) JF - Journal of Forestry Research N2 - The effects of drought on tree mortality at forest stands are not completely understood. For assessing their water supply, knowledge of the small-scale distribution of soil moisture as well as its temporal changes is a key issue in an era of climate change. However, traditional methods like taking soil samples or installing data loggers solely collect parameters of a single point or of a small soil volume. Electrical resistivity tomography (ERT) is a suitable method for monitoring soil moisture changes and has rarely been used in forests. This method was applied at two forest sites in Bavaria, Germany to obtain high-resolution data of temporal soil moisture variations. Geoelectrical measurements (2D and 3D) were conducted at both sites over several years (2015–2018/2020) and compared with soil moisture data (matric potential or volumetric water content) for the monitoring plots. The greatest variations in resistivity values that highly correlate with soil moisture data were found in the main rooting zone. Using the ERT data, temporal trends could be tracked in several dimensions, such as the interannual increase in the depth of influence from drought events and their duration, as well as rising resistivity values going along with decreasing soil moisture. The results reveal that resistivity changes are a good proxy for seasonal and interannual soil moisture variations. Therefore, 2D- and 3D-ERT are recommended as comparatively non-laborious methods for small-spatial scale monitoring of soil moisture changes in the main rooting zone and the underlying subsurface of forested sites. Higher spatial and temporal resolution allows a better understanding of the water supply for trees, especially in times of drought. KW - geoelectrical monitoring KW - forest ecology KW - hydrology KW - soil water content Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324073 SN - 1007-662X VL - 33 IS - 5 ER - TY - JOUR A1 - Ibebuchi, Chibuike Chiedozie T1 - Patterns of atmospheric circulation in Western Europe linked to heavy rainfall in Germany: preliminary analysis into the 2021 heavy rainfall episode JF - Theoretical and Applied Climatology N2 - The July 2021 heavy rainfall episode in parts of Western Europe caused devastating floods, specifically in Germany. This study examines circulation types (CTs) linked to extreme precipitation in Germany. It was investigated if the classified CTs can highlight the anomaly in synoptic patterns that contributed to the unusual July 2021 heavy rainfall in Germany. The North Atlantic Oscillation was found to be the major climatic mode related to the seasonal and inter-annual variations of most of the classified CTs. On average, wet (dry) conditions in large parts of Germany can be linked to westerly (northerly) moisture fluxes. During spring and summer seasons, the mid-latitude cyclone when located over the North Sea disrupts onshore moisture transport from the North Atlantic Ocean by westerlies driven by the North Atlantic subtropical anticyclone. The CT found to have the highest probability of being associated with above-average rainfall in large part of Germany features (i) enhancement and northward track of the cyclonic system over the Mediterranean; (ii) northward track of the North Atlantic anticyclone, further displacing poleward, the mid-latitude cyclone over the North Sea, enabling band of westerly moisture fluxes to penetrate Germany; (iii) cyclonic system over the Baltic Sea coupled with northeast fluxes of moisture to Germany; (iv) and unstable atmospheric conditions over Germany. In 2021, a spike was detected in the amplitude and frequency of occurrence of the aforementioned wet CT suggesting that in addition to the nearly stationary cut-off low over central Europe, during the July flood episode, anomalies in the CT contributed to the heavy rainfall event. KW - circulation type (CT) KW - atmospheric circulation KW - Western Europe KW - Germany KW - flood KW - heavy rainfall Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-324100 SN - 0177-798X VL - 148 IS - 1-2 ER - TY - JOUR A1 - Philipp, Marius A1 - Dietz, Andreas A1 - Ullmann, Tobias A1 - Kuenzer, Claudia T1 - A circum-Arctic monitoring framework for quantifying annual erosion rates of permafrost coasts JF - Remote Sensing N2 - This study demonstrates a circum-Arctic monitoring framework for quantifying annual change of permafrost-affected coasts at a spatial resolution of 10 m. Frequent cloud coverage and challenging lighting conditions, including polar night, limit the usability of optical data in Arctic regions. For this reason, Synthetic Aperture RADAR (SAR) data in the form of annual median and standard deviation (sd) Sentinel-1 (S1) backscatter images covering the months June–September for the years 2017–2021 were computed. Annual composites for the year 2020 were hereby utilized as input for the generation of a high-quality coastline product via a Deep Learning (DL) workflow, covering 161,600 km of the Arctic coastline. The previously computed annual S1 composites for the years 2017 and 2021 were employed as input data for the Change Vector Analysis (CVA)-based coastal change investigation. The generated DL coastline product served hereby as a reference. Maximum erosion rates of up to 67 m per year could be observed based on 400 m coastline segments. Overall highest average annual erosion can be reported for the United States (Alaska) with 0.75 m per year, followed by Russia with 0.62 m per year. Out of all seas covered in this study, the Beaufort Sea featured the overall strongest average annual coastal erosion of 1.12 m. Several quality layers are provided for both the DL coastline product and the CVA-based coastal change analysis to assess the applicability and accuracy of the output products. The predicted coastal change rates show good agreement with findings published in previous literature. The proposed methods and data may act as a valuable tool for future analysis of permafrost loss and carbon emissions in Arctic coastal environments. KW - permafrost KW - coastal erosion KW - circum-Arctic KW - deep learning KW - change vector analysis KW - Google Earth Engine KW - synthetic aperture RADAR Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-304447 SN - 2072-4292 VL - 15 IS - 3 ER - TY - JOUR A1 - Kacic, Patrick A1 - Thonfeld, Frank A1 - Gessner, Ursula A1 - Kuenzer, Claudia T1 - Forest structure characterization in Germany: novel products and analysis based on GEDI, Sentinel-1 and Sentinel-2 data JF - Remote Sensing N2 - Monitoring forest conditions is an essential task in the context of global climate change to preserve biodiversity, protect carbon sinks and foster future forest resilience. Severe impacts of heatwaves and droughts triggering cascading effects such as insect infestation are challenging the semi-natural forests in Germany. As a consequence of repeated drought years since 2018, large-scale canopy cover loss has occurred calling for an improved disturbance monitoring and assessment of forest structure conditions. The present study demonstrates the potential of complementary remote sensing sensors to generate wall-to-wall products of forest structure for Germany. The combination of high spatial and temporal resolution imagery from Sentinel-1 (Synthetic Aperture Radar, SAR) and Sentinel-2 (multispectral) with novel samples on forest structure from the Global Ecosystem Dynamics Investigation (GEDI, LiDAR, Light detection and ranging) enables the analysis of forest structure dynamics. Modeling the three-dimensional structure of forests from GEDI samples in machine learning models reveals the recent changes in German forests due to disturbances (e.g., canopy cover degradation, salvage logging). This first consistent data set on forest structure for Germany from 2017 to 2022 provides information of forest canopy height, forest canopy cover and forest biomass and allows estimating recent forest conditions at 10 m spatial resolution. The wall-to-wall maps of the forest structure support a better understanding of post-disturbance forest structure and forest resilience. KW - forest KW - forest structure Germany KW - canopy height KW - Global Ecosystem Dynamics Investigation KW - GEDI KW - Sentinel-1 KW - Sentinel-2 KW - random forest regression Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-313727 SN - 2072-4292 VL - 15 IS - 8 ER - TY - THES A1 - Philipp, Marius Balthasar T1 - Quantifying the Effects of Permafrost Degradation in Arctic Coastal Environments via Satellite Earth Observation T1 - Quantifizierung der Effekte von Permafrost Degradation in Arktischen Küstenregionen mittels Satelliten-gestützter Erdbeobachtung N2 - Permafrost degradation is observed all over the world as a consequence of climate change and the associated Arctic amplification, which has severe implications for the environment. Landslides, increased rates of surface deformation, rising likelihood of infrastructure damage, amplified coastal erosion rates, and the potential turnover of permafrost from a carbon sink to a carbon source are thereby exemplary implications linked to the thawing of frozen ground material. In this context, satellite earth observation is a potent tool for the identification and continuous monitoring of relevant processes and features on a cheap, long-term, spatially explicit, and operational basis as well as up to a circumpolar scale. A total of 325 articles published in 30 different international journals during the past two decades were investigated on the basis of studied environmental foci, remote sensing platforms, sensor combinations, applied spatio-temporal resolutions, and study locations in an extensive review on past achievements, current trends, as well as future potentials and challenges of satellite earth observation for permafrost related analyses. The development of analysed environmental subjects, utilized sensors and platforms, and the number of annually published articles over time are addressed in detail. Studies linked to atmospheric features and processes, such as the release of greenhouse gas emissions, appear to be strongly under-represented. Investigations on the spatial distribution of study locations revealed distinct study clusters across the Arctic. At the same time, large sections of the continuous permafrost domain are only poorly covered and remain to be investigated in detail. A general trend towards increasing attention in satellite earth observation of permafrost and related processes and features was observed. The overall amount of published articles hereby more than doubled since the year 2015. New sources of satellite data, such as the Sentinel satellites and the Methane Remote Sensing LiDAR Mission (Merlin), as well as novel methodological approaches, such as data fusion and deep learning, will thereby likely improve our understanding of the thermal state and distribution of permafrost, and the effects of its degradation. Furthermore, cloud-based big data processing platforms (e.g. Google Earth Engine (GEE)) will further enable sophisticated and long-term analyses on increasingly larger scales and at high spatial resolutions. In this thesis, a specific focus was put on Arctic permafrost coasts, which feature increasing vulnerability to environmental parameters, such as the thawing of frozen ground, and are therefore associated with amplified erosion rates. In particular, a novel monitoring framework for quantifying Arctic coastal erosion rates within the permafrost domain at high spatial resolution and on a circum-Arctic scale is presented within this thesis. Challenging illumination conditions and frequent cloud cover restrict the applicability of optical satellite imagery in Arctic regions. In order to overcome these limitations, Synthetic Aperture RADAR (SAR) data derived from Sentinel-1 (S1), which is largely independent from sun illumination and weather conditions, was utilized. Annual SAR composites covering the months June–September were combined with a Deep Learning (DL) framework and a Change Vector Analysis (CVA) approach to generate both a high-quality and circum-Arctic coastline product as well as a coastal change product that highlights areas of erosion and build-up. Annual composites in the form of standard deviation (sd) and median backscatter were computed and used as inputs for both the DL framework and the CVA coastal change quantification. The final DL-based coastline product covered a total of 161,600 km of Arctic coastline and featured a median accuracy of ±6.3 m to the manually digitized reference data. Annual coastal change quantification between 2017–2021 indicated erosion rates of up to 67 m per year for some areas based on 400 m coastal segments. In total, 12.24% of the investigated coastline featured an average erosion rate of 3.8 m per year, which corresponds to 17.83 km2 of annually eroded land area. Multiple quality layers associated to both products, the generated DL-coastline and the coastal change rates, are provided on a pixel basis to further assess the accuracy and applicability of the proposed data, methods, and products. Lastly, the extracted circum-Arctic erosion rates were utilized as a basis in an experimental framework for estimating the amount of permafrost and carbon loss as a result of eroding permafrost coastlines. Information on permafrost fraction, Active Layer Thickness (ALT), soil carbon content, and surface elevation were thereby combined with the aforementioned erosion rates. While the proposed experimental framework provides a valuable outline for quantifying the volume loss of frozen ground and carbon release, extensive validation of the utilized environmental products and resulting volume loss numbers based on 200 m segments are necessary. Furthermore, data of higher spatial resolution and information of carbon content for deeper soil depths are required for more accurate estimates. N2 - Als Folge des Klimawandels und der damit verbundenen „Arctic Amplification“ wird weltweit eine Degradation des Dauerfrostbodens (Permafrost) beobachtet, welche schwerwiegende Auswirkungen auf die Umwelt hat. Erdrutsche, erhöhte Oberflächen- verformungsraten, eine zunehmende Wahrscheinlichkeit von Infrastrukturschäden, verstärkte Küstenerosionsraten und die potenzielle Umwandlung von Permafrost von einer Kohlenstoffsenke in eine Kohlenstoffquelle sind dabei beispielhafte Auswirkun- gen im Zusammenhang mit dem Auftauen von gefrorenem Bodenmaterial. In diesem Kontext ist die Satelliten-gestützte Erdbeobachtung ein wirkmächtiges Werkzeug zur Identifizierung und kontinuierlichen Überwachung relevanter Prozesse und Merkmale auf einer kostengünstigen, langfristigen, räumlich expliziten und operativen Basis und auf einem zirkumpolaren Maßstab. Insgesamt 325 Artikel, die in den letzten zwei Jahrzehnten in 30 verschiedenen internationalen Zeitschriften veröffentlicht wurden, wurden auf Basis der adressierten Umweltschwerpunkte, Fernerkundungsplattformen, Sensorkombinationen, angewand- ten raum-zeitlichen Auflösungen und den Studienorten in einem umfassenden Überblick über vergangene Errungenschaften und aktuelle Trends untersucht. Zusätzlich wur- den zukünftige Potenziale und Herausforderungen der Satelliten-Erdbeobachtung für Permafrost-bezogene Analysen diskutiert. Auf die zeitliche Entwicklung der un- tersuchten Umweltthemen, eingesetzten Sensoren und Satelliten-Plattformen sowie die Zahl der jährlich erscheinenden Artikel wurde detailliert eingegangen. Studien zu atmosphärischen Eigenschaften und Prozessen, wie etwa der Freisetzung von Treibhaus- gasemissionen, waren stark unterrepräsentiert. Deutliche geografische Schlüssel-Gebiete, auf welche sich der Großteil der Studien konzentrierte, konnten in Untersuchungen zur räumlichen Verteilung der Studienorte identifiziert werden. Gleichzeitig sind große Teile des kontinuierlichen Permafrost-Gebiets nur spärlich abgedeckt und müssen noch im Detail untersucht werden. Es wurde ein allgemeiner Trend zu einer zunehmenden Aufmerksamkeit bezüglich der Satelliten-gestützten Erdbeobachtung von Permafrost und verwandten Prozessen und Merkmalen beobachtet. Die Gesamtzahl der veröf- fentlichten Artikel hat sich dabei seit dem Jahr 2015 mehr als verdoppelt. Neue Quellen für Satellitendaten, wie beispielweise die Sentinel-Satelliten und die Methane Remote Sensing LiDAR Mission (Merlin), sowie neuartige methodische Ansätze, wie Datenfusion und Deep Learning, werden dabei voraussichtlich unser Verständnis bzgl. des thermischen Zustands und der Verteilung von Permafrost-Vorkommen sowie die Auswirkungen seines Auftauens verbessern. Darüber hinaus werden Cloud-basierte Big-Data-Verarbeitungsplattformen (z.B. Google Earth Engine (GEE)) anspruchsvolle und langfristige Analysen in immer größeren Maßstäben und mit hoher räumlicher Auflösung erleichtern. In dieser Arbeit wurde ein besonderer Fokus auf arktische Permafrost-Küsten gelegt, die eine zunehmende Vulnerabilität gegenüber Umweltparametern wie dem Auftauen von gefrorenem Boden aufweisen und daher von verstärkten Erosionsraten betroffen sind. Ein neuartiger Ansatz zur Quantifizierung der arktischen Küstene- rosion innerhalb des Permafrost-Gebiets mit hoher räumlicher Auflösung und auf zirkum-arktischem Maßstab wird in dieser Dissertation präsentiert. Schwierige Be- leuchtungsbedingungen und häufige Bewölkung schränken die Anwendbarkeit optischer Satellitenbilder in arktischen Regionen ein. Um diese Einschränkungen zu überwinden, wurden Synthetic Aperture RADAR (SAR) Daten von Sentinel-1 (S1) verwendet, die weitgehend unabhängig von Sonneneinstrahlung und Wetterbedingungen sind. Jährli- che SAR-Komposite, welche die Monate Juni bis September abdecken, wurden mit einem Deep Learning (DL)-Ansatz und einer Change Vector Analysis (CVA)-Methode kombiniert, um sowohl ein qualitativ hochwertiges und zirkum-arktisches Küstenli- nienprodukt als auch ein Produkt für die Änderungsraten (Erosion und küstennahe Aggregation von Sedimenten) der Küste zu generieren. Jährliche Satelliten-Komposite in Form von der Standardabweichung (sd) und des Medians der SAR Rückstreuung wurden hierbei berechnet und als Eingabedaten sowohl für den DL-Ansatz als auch für die Quantifizierung der CVA-basierten Küstenänderung verwendet. Das endgül- tige DL-basierte Küstenlinienprodukt deckt insgesamt 161.600 km der arktischen Küstenlinie ab und wies eine Median-Abweichung von ±6,3 m gegenüber den ma- nuell digitalisierten Referenzdaten auf. Im Zuge der Quantifizierung von jährlichen Küstenveränderungen zwischen 2017 und 2021 konnten Erosionsraten von bis zu 67 m pro Jahr und basierend auf 400 m Küstenabschnitten identifiziert werden. Insgesamt wiesen 12,24% der untersuchten Küstenlinie eine durchschnittliche Erosionsrate von 3,8 m pro Jahr auf, was einer jährlichen erodierten Landfläche von 17,83 km2 entspricht. Mehrere Qualitäts-Datensätze, die beiden Produkten zugeordnet sind, wurden auf Pixelbasis bereitgestellt, um die Genauigkeit und Anwendbarkeit der präsentierten Daten, Methoden und Produkte weiter einordnen zu können. Darüber hinaus wurden die extrahierten zirkum-arktischen Erosionsraten als Grund- lage in einem experimentellen Ansatz verwendet, um die Menge an Permafrost-Verlust und Kohlenstofffreistzung als Konsequenz der erodierten Permafrost-Küsten abzu- schätzen. Dabei wurden Informationen zu Permafrost-Anteil, Active Layer Thickness (ALT), Höhenmodellen und der Menge an im Boden gespeichertem Kohlenstoff mit den oben genannten Erosionsraten kombiniert. Während der präsentierte experimentelle Ansatz einen wertvollen Ausgangspunkt für die Quantifizierung des Volumenverlusts von gefrorenem Boden und der Kohlenstofffreisetzung darstellt, ist eine umfassende Validierung der verwendeten Umweltprodukte und der resultierenden Volumenzah- len erforderlich. Zusätzlich werden für genauere Abschätzungen Daten mit höherer räumlicher Auflösung und Informationen zum Kohlenstoffgehalt für tiefere Bodentiefen benötigt. KW - Dauerfrostboden KW - Synthetische Apertur KW - Deep learning KW - Erosion KW - Satellit KW - Synthetic Aperture RADAR KW - Circumpolar KW - Arctic KW - Permafrost KW - Satellite Earth Observation KW - Change Vector Analysis Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-345634 ER - TY - JOUR A1 - Reiners, Philipp A1 - Sobrino, José A1 - Kuenzer, Claudia T1 - Satellite-derived land surface temperature dynamics in the context of global change — a review JF - Remote Sensing N2 - Satellite-derived Land Surface Temperature (LST) dynamics have been increasingly used to study various geophysical processes. This review provides an extensive overview of the applications of LST in the context of global change. By filtering a selection of relevant keywords, a total of 164 articles from 14 international journals published during the last two decades were analyzed based on study location, research topic, applied sensor, spatio-temporal resolution and scale and employed analysis methods. It was revealed that China and the USA were the most studied countries and those that had the most first author affiliations. The most prominent research topic was the Surface Urban Heat Island (SUHI), while the research topics related to climate change were underrepresented. MODIS was by far the most used sensor system, followed by Landsat. A relatively small number of studies analyzed LST dynamics on a global or continental scale. The extensive use of MODIS highly determined the study periods: A majority of the studies started around the year 2000 and thus had a study period shorter than 25 years. The following suggestions were made to increase the utilization of LST time series in climate research: The prolongation of the time series by, e.g., using AVHRR LST, the better representation of LST under clouds, the comparison of LST to traditional climate change measures, such as air temperature and reanalysis variables, and the extension of the validation to heterogenous sites. KW - remote sensing KW - land surface temperature KW - temperature KW - dynamics KW - global change KW - climate change KW - global warming KW - earth observation KW - review Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-311120 SN - 2072-4292 VL - 15 IS - 7 ER - TY - JOUR A1 - Dhillon, Maninder Singh A1 - Kübert-Flock, Carina A1 - Dahms, Thorsten A1 - Rummler, Thomas A1 - Arnault, Joel A1 - Steffan-Dewenter, Ingolf A1 - Ullmann, Tobias T1 - Evaluation of MODIS, Landsat 8 and Sentinel-2 data for accurate crop yield predictions: a case study using STARFM NDVI in Bavaria, Germany JF - Remote Sensing N2 - The increasing availability and variety of global satellite products and the rapid development of new algorithms has provided great potential to generate a new level of data with different spatial, temporal, and spectral resolutions. However, the ability of these synthetic spatiotemporal datasets to accurately map and monitor our planet on a field or regional scale remains underexplored. This study aimed to support future research efforts in estimating crop yields by identifying the optimal spatial (10 m, 30 m, or 250 m) and temporal (8 or 16 days) resolutions on a regional scale. The current study explored and discussed the suitability of four different synthetic (Landsat (L)-MOD13Q1 (30 m, 8 and 16 days) and Sentinel-2 (S)-MOD13Q1 (10 m, 8 and 16 days)) and two real (MOD13Q1 (250 m, 8 and 16 days)) NDVI products combined separately to two widely used crop growth models (CGMs) (World Food Studies (WOFOST), and the semi-empiric Light Use Efficiency approach (LUE)) for winter wheat (WW) and oil seed rape (OSR) yield forecasts in Bavaria (70,550 km\(^2\)) for the year 2019. For WW and OSR, the synthetic products’ high spatial and temporal resolution resulted in higher yield accuracies using LUE and WOFOST. The observations of high temporal resolution (8-day) products of both S-MOD13Q1 and L-MOD13Q1 played a significant role in accurately measuring the yield of WW and OSR. For example, L- and S-MOD13Q1 resulted in an R\(^2\) = 0.82 and 0.85, RMSE = 5.46 and 5.01 dt/ha for WW, R\(^2\) = 0.89 and 0.82, and RMSE = 2.23 and 2.11 dt/ha for OSR using the LUE model, respectively. Similarly, for the 8- and 16-day products, the simple LUE model (R\(^2\) = 0.77 and relative RMSE (RRMSE) = 8.17%) required fewer input parameters to simulate crop yield and was highly accurate, reliable, and more precise than the complex WOFOST model (R\(^2\) = 0.66 and RRMSE = 11.35%) with higher input parameters. Conclusively, both S-MOD13Q1 and L-MOD13Q1, in combination with LUE, were more prominent for predicting crop yields on a regional scale than the 16-day products; however, L-MOD13Q1 was advantageous for generating and exploring the long-term yield time series due to the availability of Landsat data since 1982, with a maximum resolution of 30 m. In addition, this study recommended the further use of its findings for implementing and validating the long-term crop yield time series in different regions of the world. KW - MODIS KW - Sentinel-2 KW - Landsat 8 KW - sustainable agriculture KW - decision-making KW - winter wheat KW - oil seed rape KW - resolution Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-311132 SN - 2072-4292 VL - 15 IS - 7 ER - TY - JOUR A1 - Bender, Oliver A1 - Roth, Charlotte E. A1 - Job, Hubert T1 - Protected areas and population development in the alps JF - eco.mont : Journal on Protected Mountain Areas Research and Management N2 - Nearly a quarter of the Alpine area is covered by a dense network of large protected areas (LPAs) of the four categories national park(NP), biosphere reserve (BR), nature park and world natural heritage site (WNHS). From the time of early industrialization, the Alpine area has undergone a mixed and increasingly polarized demographic development between the poles of immigration and emigration. This article investigates the possible mutual impact of population development and the existence of LPAs. The research design includes a quantitative survey of all Alpine LPAs in terms of their population development and the structure of immigration in the first decade of the 21st century. This will be linked with qualitative expert interviews in four selected NPs. The overall results allow an interpretation of the statistical correlations between type of LPA and migration. KW - geography KW - amenity migration KW - national parks KW - population KW - protected areas KW - regional development Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-181901 VL - 9 IS - Special issue ER - TY - JOUR A1 - Senaratne, Hansi A1 - Mühlbauer, Martin A1 - Kiefl, Ralph A1 - Cárdenas, Andrea A1 - Prathapan, Lallu A1 - Riedlinger, Torsten A1 - Biewer, Carolin A1 - Taubenböck, Hannes T1 - The Unseen — an investigative analysis of thematic and spatial coverage of news on the ongoing refugee crisis in West Africa JF - ISPRS International Journal of Geo-Information N2 - The fastest growing regional crisis is happening in West Africa today, with over 8 million people considered persons of concern. A culmination of identity politics, climate-driven disasters, and extreme poverty has led to this humanitarian crisis in the region and is exacerbated by a lack of political will and misplaced media attention. The current state of the art does not present sufficient investigations of the thematic and spatial coverage of news media of this crisis in this region. This paper studies the spatial coverage of this crisis as reported in the media, and the themes associated with those locations, based on a curated dataset. For the time frame 12 March to 15 September 2021, 2017 news articles related to the refugee crisis in West Africa were examined and manually coded based on (1) the geographical locations mentioned in each article; (2) the themes found in the articles in reference to a location (e.g., Relocation of people in Abuja). The dataset introduces a thematic dimension, as never achieved before, to the conflict-ridden areas in West Africa. A comparative analysis with UNHCR (United Nations High Commissioner for Refugees) data showed that 96.8% of refugee-related locations in West Africa were not covered by news during the considered time frame. Contrastingly, 80.4% of locations mentioned in the news do not appear in the UNHCR repository. Most news articles published during this time frame reported on Development aid or Political statements. Linear multiple regression analysis showed GDP per capita and political stability to be among the most influential determinants of news coverage. KW - West African refugee crisis KW - news media reporting KW - spatio-thematic coverage Y1 - 2023 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-313607 SN - 2220-9964 VL - 12 IS - 4 ER - TY - JOUR A1 - Latifi, Hooman A1 - Holzwarth, Stefanie A1 - Skidmore, Andrew A1 - Brůna, Josef A1 - Červenka, Jaroslav A1 - Darvishzadeh, Roshanak A1 - Hais, Martin A1 - Heiden, Uta A1 - Homolová, Lucie A1 - Krzystek, Peter A1 - Schneider, Thomas A1 - Starý, Martin A1 - Wang, Tiejun A1 - Müller, Jörg A1 - Heurich, Marco T1 - A laboratory for conceiving Essential Biodiversity Variables (EBVs)—The ‘Data pool initiative for the Bohemian Forest Ecosystem’ JF - Methods in Ecology and Evolution N2 - Effects of climate change‐induced events on forest ecosystem dynamics of composition, function and structure call for increased long‐term, interdisciplinary and integrated research on biodiversity indicators, in particular within strictly protected areas with extensive non‐intervention zones. The long‐established concept of forest supersites generally relies on long‐term funds from national agencies and goes beyond the logistic and financial capabilities of state‐ or region‐wide protected area administrations, universities and research institutes. We introduce the concept of data pools as a smaller‐scale, user‐driven and reasonable alternative to co‐develop remote sensing and forest ecosystem science to validated products, biodiversity indicators and management plans. We demonstrate this concept with the Bohemian Forest Ecosystem Data Pool, which has been established as an interdisciplinary, international data pool within the strictly protected Bavarian Forest and Šumava National Parks and currently comprises 10 active partners. We demonstrate how the structure and impact of the data pool differs from comparable cases. We assessed the international influence and visibility of the data pool with the help of a systematic literature search and a brief analysis of the results. Results primarily suggest an increase in the impact and visibility of published material during the life span of the data pool, with highest visibilities achieved by research conducted on leaf traits, vegetation phenology and 3D‐based forest inventory. We conclude that the data pool results in an efficient contribution to the concept of global biodiversity observatory by evolving towards a training platform, functioning as a pool of data and algorithms, directly communicating with management for implementation and providing test fields for feasibility studies on earth observation missions. KW - bohemian forest ecosystem KW - data pool KW - forest ecosystem science KW - remote sensing KW - remote sensing‐enabled essential biodiversity variables Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-262743 VL - 12 IS - 11 ER - TY - THES A1 - Fekete, Alexander T1 - Urban Disaster Resilience and Critical Infrastructure T1 - Urbane Katastrophen-Resilienz und Kritische Infrastruktur N2 - Urban areas are population, culture and infrastructure concentration points. Electricity blackouts or interruptions of water supply severely affect people when happening unexpected and at large scale. Interruptions of such infrastructure supply services alone have the potential to trigger crises. But when happening in concert with or as a secondary effect of an earthquake, for example, the crisis situation is often aggravated. This is the case for any country, but it has been observed that even highly industrialised countries face severe risks when their degree of acquired dependency on services of what is termed Critical Infrastructure results in even bigger losses when occurring unexpectedly in a setting that usually has high reliability of services. N2 - Die Forschung zu Naturgefahren und Katastrophen hat sich in den vergangenen Jahren weniger mit der reinen Erforschung der Gefahrenseite, sondern zunehmend mit Auswirkungsprozessen von Krisen und Katastrophen auf Gesellschaft, Umwelt, Politik, und andere Bereichen befasst. Da sich die Gesellschaft immer weiter vernetzt, sei es durch moderne Technologien, Warenströme oder Kommunikation, haben sich auch die Auswirkung von beispielsweise Naturkatastrophen zu global spürbaren Auswirkungen hin entwickelt. Das Habilitationsvorhaben befasst sich mit Städten und Siedlungsformen als Bündelungspunkten mehrerer Risiken. International bekannt geworden ist dieses Thema unter anderem unter dem Begriff „Resiliente Stadt“. In Städten und anderen Sicherungsräumen bündeln sich nicht nur Siedlungen und Bevölkerung sondern auch Infrastrukturknotenpunkte. Städte sind also nicht nur Orte von möglichen Naturkatastrophen-Einwirkungen, sondern auch Orte in denen sich Ausfälle beispielsweise der Elektrizitätsversorgung, der Wasserversorgung oder anderer lebenswichtiger Versorgungsdienstleistungen besonders spürbar bemerkbar machen. Lebenswichtige Versorgungseinrichtungen werden seit Mitte der Neunzigerjahre auch unter dem Themenfeld „Kritische Infrastrukturen“ untersucht. Die Forschung hierzu wurde vor allem durch einzelne Vorfälle, wie etwa Bombenanschlägen in den USA, Internet Angriffen oder auch durch längere Stromausfälle, beispielsweise durch Hochwasser, auch in Deutschland ein zunehmend bekanntes Thema. Dieses Themenfeld wurde einerseits durch die Politik und andererseits durch die Wissenschaft aufgegriffen und vorangetrieben. Interessanterweise haben sich jedoch die Forschungsbereiche Naturgefahrenforschung und kritische Infrastruktur weitgehen getrennt entwickelt. Diese Arbeit untersucht daher insbesondere, welche Wechselwirkungen zwischen diesen beiden Bereichen bestehen, und entwickelt Methoden, um sowohl qualitative als auch quantitative Ansätze zur Identifizierung, zur Beobachtung, und zur vergleichenden Analyse zu entwickeln. Bei der Methodenentwicklung stützt sich die Arbeit auf die Entwicklung räumlicher Verwundbarkeitsindikatoren, die im Bereich der Naturgefahrenforschung entwickelt wurde, und untersucht die weitere Entwicklung hin zu Resilienz-Analysen. Hierbei werden sowohl physikalische Faktoren zur Bemessung von Katastrophenauswirkungen, zum Beispiel Exposition und Niederschlagsmengen mit demographischen Indikatoren verknüpft. Im Bereich kritischer Infrastrukturen kommt noch eine weitere Methodik hinzu: die Einschätzung der Kritikalität; damit ist die Bedeutung der Auswirkungen von Versorgungsausfällen für die Gesellschaft gemeint. Dabei werden auf der einen Seite sowohl Schwachpunkte und Schwachstellen der Versorgungsnetze identifiziert, auf der anderen Seite werden Auswirkungen auf die Gesellschaft, wie etwa auf physiologische Überlebensfunktionen, Nahrungsgrundlagen, Wirtschafts- und Wertesysteme untersucht. KW - Risikomanagement KW - Risikoanalyse KW - Naturgefahr KW - Naturkatastrophe KW - Resilienz KW - Kritische Infrastruktur KW - Urbane Resilienz KW - Resiliente Stadt Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-163251 SN - 978-3-946573-13-5 ER - TY - JOUR A1 - Dietrich, Laura A1 - Meister, Julia A1 - Dietrich, Oliver A1 - Notroff, Jens A1 - Kiep, Janika A1 - Heeb, Julia A1 - Beuger, André A1 - Schütt, Brigitta T1 - Cereal processing at Early Neolithic Göbekli Tepe, southeastern Turkey JF - PLoS ONE N2 - We analyze the processing of cereals and its role at Early Neolithic Göbekli Tepe, southeastern Anatolia (10th / 9th millennium BC), a site that has aroused much debate in archaeological discourse. To date, only zooarchaeological evidence has been discussed in regard to the subsistence of its builders. Göbekli Tepe consists of monumental round to oval buildings, erected in an earlier phase, and smaller rectangular buildings, built around them in a partially contemporaneous and later phase. The monumental buildings are best known as they were in the focus of research. They are around 20 m in diameter and have stone pillars that are up to 5.5 m high and often richly decorated. The rectangular buildings are smaller and–in some cases–have up to 2 m high, mostly undecorated, pillars. Especially striking is the number of tools related to food processing, including grinding slabs/bowls, handstones, pestles, and mortars, which have not been studied before. We analyzed more than 7000 artifacts for the present contribution. The high frequency of artifacts is unusual for contemporary sites in the region. Using an integrated approach of formal, experimental, and macro- / microscopical use-wear analyses we show that Neolithic people at Göbekli Tepe have produced standardized and efficient grinding tools, most of which have been used for the processing of cereals. Additional phytolith analysis confirms the massive presence of cereals at the site, filling the gap left by the weakly preserved charred macro-rests. The organization of work and food supply has always been a central question of research into Göbekli Tepe, as the construction and maintenance of the monumental architecture would have necessitated a considerable work force. Contextual analyses of the distribution of the elements of the grinding kit on site highlight a clear link between plant food preparation and the rectangular buildings and indicate clear delimitations of working areas for food production on the terraces the structures lie on, surrounding the circular buildings. There is evidence for extensive plant food processing and archaeozoological data hint at large-scale hunting of gazelle between midsummer and autumn. As no large storage facilities have been identified, we argue for a production of food for immediate use and interpret these seasonal peaks in activity at the site as evidence for the organization of large work feasts. KW - Specimen grinding KW - Archaeology KW - Neolithic period KW - Sediment KW - Equipment KW - Stratigraphy KW - Limestone KW - Meat Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-201504 VL - 14 IS - 5 ER - TY - JOUR A1 - Meyer, Constantin A1 - Peters, Jan Christoph A1 - Thiel, Michael A1 - Rathmann, Joachim A1 - Job, Hubert T1 - Monitoring von Freiflächeninanspruchnahme und -versiegelung für eine nachhaltige Raumentwicklung in Bayern JF - Raumforschung und Raumordnung JF - Spatial Research and Planning N2 - Im Freistaat Bayern wird intensiv diskutiert, wie die nach wie vor hohe Freiflächeninanspruchnahme für Siedlungs- und Verkehrszwecke reduziert werden kann. Wissenschaftliche Grundlage für Steuerungsansätze in der Stadt- und Regionalentwicklung sollte ein verbessertes staatliches Flächenmonitoring sein, welches über die amtliche Statistik und deren Hauptindikator "Siedlungs- und Verkehrsfläche" hinaus auch die qualitative Dimension der Flächeninanspruchnahme einbezieht. Dafür stellt dieser Beitrag methodische Erweiterungsansätze für das Flächenmonitoring vor, welche kleinräumige Analysen der Zersiedelung, Freiraumstruktur, Flächenversiegelung und Ökosystemleistungen am Beispiel des Landkreises Rhön-Grabfeld aufzeigen. Diese werden im Kontext der Debatte zu Ursachen und Steuerung der Freiflächeninanspruchnahme sowie zu aktuellen Anforderungen an das Flächenmonitoring diskutiert. Betont wird deren Bedeutung für das Monitoring rechtlicher Vorgaben und politischer Ziele zur nachhaltigen Flächennutzung. N2 - In the federal state of Bavaria, there is currently intensive discussion on how land consumption for settlement and transport purposes can be reduced in the long term. In order to provide a solid scientific basis for steering instruments in urban and regional development, the official land use monitoring should be improved by including also the qualitative and structural dimension of land consumption in addition to existing official statistics and their main indicator ‘settlement and traffic area’. For this purpose, the paper presents methodological extensions, which show small-scale analyses of urban sprawl, open space structure, soil sealing and ecosystem services using the example of the district of Rhön-Grabfeld. These methodological extensions are discussed in the context of the relevant debates on the causes and steering of land consumption as well as on current requirements for land use monitoring, emphasising their importance for the monitoring of legal guidelines and political objectives on sustainable land use. T2 - Monitoring of land consumption and soil sealing as a contribution to sustainable spatial development in Bavaria KW - Bayern KW - Flächenmonitoring KW - Freiraumstruktur KW - Ökosystemleistungen KW - Siedlungs-und Verkehrsfläche KW - Zersiedelung KW - Bavaria KW - Ecosystem services KW - Land use monitoring KW - Open spaces KW - Settlement and traffic area KW - Urban sprawl Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-261622 VL - 79 IS - 2 ER - TY - JOUR A1 - Rösch, Manfred A1 - Biester, Harald A1 - Bogenrieder, Arno A1 - Eckmeier, Eileen A1 - Ehrmann, Otto A1 - Gerlach, Renate A1 - Hall, Mathias A1 - Hartkopf-Fröder, Christoph A1 - Herrmann, Ludger A1 - Kury, Birgit A1 - Lechterbeck, Jutta A1 - Schier, Wolfram A1 - Schulz, Erhard T1 - Late neolithic agriculture in temperate Europe—a long-term experimental approach JF - Land N2 - Long-term slash-and-burn experiments, when compared with intensive tillage without manuring, resulted in a huge data set relating to potential crop yields, depending on soil quality, crop type, and agricultural measures. Cultivation without manuring or fallow phases did not produce satisfying yields, and mono-season cropping on freshly cleared and burned plots resulted in rather high yields, comparable to those produced during modern industrial agriculture - at least ten-fold the ones estimated for the medieval period. Continuous cultivation on the same plot, using imported wood from adjacent areas as fuel, causes decreasing yields over several years. The high yield of the first harvest of a slash-and-burn agriculture is caused by nutrient input through the ash produced and mobilization from the organic matter of the topsoil, due to high soil temperatures during the burning process and higher topsoil temperatures due to the soil’s black surface. The harvested crops are pure, without contamination of any weeds. Considering the amount of work required to fight weeds without burning, the slash-and-burn technique yields much better results than any other tested agricultural approach. Therefore, in dense woodland, without optimal soils and climate, slash-and-burn agriculture seems to be the best, if not the only, feasible method to start agriculture, for example, during the Late Neolithic, when agriculture expanded from the loess belt into landscapes less suitable for agriculture. Extensive and cultivation with manuring is more practical in an already-open landscape and with a denser population, but its efficiency in terms of the ratio of the manpower input to food output, is worse. Slash-and-burn agriculture is not only a phenomenon of temperate European agriculture during the Neolithic, but played a major role in land-use in forested regions worldwide, creating anthromes on a huge spatial scale. KW - Neolithic agriculture KW - experimental archaeology KW - slash-and-burn KW - temperate Europe Y1 - 2017 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-198103 SN - 2073-445X VL - 6 IS - 1 ER - TY - JOUR A1 - Ullmann, Tobias A1 - Möller, Eric A1 - Baumhauer, Roland A1 - Lange-Athinodorou, Eva A1 - Meister, Julia T1 - A new Google Earth Engine tool for spaceborne detection of buried palaeogeographical features – examples from the Nile Delta (Egypt) JF - E&G Quaternary Science Journal N2 - No abstract available. KW - Google Earth KW - Nile Delta (Egypt) KW - paleogeography Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-300164 VL - 71 IS - 2 ER - TY - JOUR A1 - Ullmann, Tobias A1 - Nill, Leon A1 - Schiestl, Robert A1 - Trappe, Julian A1 - Lange-Athinodorou, Eva A1 - Baumhauer, Roland A1 - Meister, Julia T1 - Mapping buried paleogeographical features of the Nile Delta (Egypt) using the Landsat archive JF - E&G Quartnerny Science Journal N2 - The contribution highlights the use of Landsat spectral-temporal metrics (STMs) for the detection of surface anomalies that are potentially related to buried near-surface paleogeomorphological deposits in the Nile Delta (Egypt), in particular for a buried river branch close to Buto. The processing was completed in the Google Earth Engine (GEE) for the entire Nile Delta and for selected seasons of the year (summer/winter) using Landsat data from 1985 to 2019. We derived the STMs of the tasseled cap transformation (TC), the Normalized Difference Wetness Index (NDWI), and the Normalized Difference Vegetation Index (NDVI). These features were compared to historical topographic maps of the Survey of Egypt, CORONA imagery, the digital elevation model of the TanDEM-X mission, and modern high-resolution satellite imagery. The results suggest that the extent of channels is best revealed when differencing the median NDWI between summer (July/August) and winter (January/February) seasons (ΔNDWI). The observed difference is likely due to lower soil/plant moisture during summer, which is potentially caused by coarser-grained deposits and the morphology of the former levee. Similar anomalies were found in the immediate surroundings of several Pleistocene sand hills (“geziras”) and settlement mounds (“tells”) of the eastern delta, which allowed some mapping of the potential near-surface continuation. Such anomalies were not observed for the surroundings of tells of the western Nile Delta. Additional linear and meandering ΔNDWI anomalies were found in the eastern Nile Delta in the immediate surroundings of the ancient site of Bubastis (Tell Basta), as well as several kilometers north of Zagazig. These anomalies might indicate former courses of Nile river branches. However, the ΔNDWI does not provide an unambiguous delineation. N2 - Die Rekonstruktion der Paläotopographie und -hydrographie des Nildeltas spielt für landschaftsarchäologische Fragestellungen eine zentrale Rolle, da die antike Siedlungsaktivität stark von der Dynamik des antiken Flussnetzes beeinflusst war. Für viele Bereiche des Deltas ist die Lage antiker Flussarme jedoch unbekannt, da diese im Laufe der Zeit verlandet und heute nicht mehr eindeutig im Landschaftsbild erkennbar sind. In diesem Kontext erlauben moderne Fernerkundungsdaten eine flächendeckende Untersuchung und ermöglichen Anomalien der Landbedeckung und Diskontinuitäten der Oberflächenmorphologie zu identifizieren, wodurch wertvolle Hinweise zur paläogeomorphologischen Situation gewonnen werden können. Zur Detektion solcher Anomalien wird in diesem Beitrag das Landsat Archiv genutzt, wobei verschiedene spektrale und zeitlich-räumliche Metriken für das gesamte Nildelta (Ägypten) für den Zeitraum 1985 bis 2019 in der Google Earth Engine berechnet wurden. Die Merkmale der Merkmale der Tasseled Cap Transformation (TC), des Normalized Difference Wetness Index (NDWI) und des Normalized Difference Vegetation Index (NDVI) wurden analysiert und mit historischen topographischen Karten des Survey of Egypt, CORONA-Bildern, dem digitalen Höhenmodell der TanDEM-X-Mission und modernen Satellitenbildern verglichen. Die Ergebnisse der Zeitserienanalyse zeigen die Lage eines verlandeten Flussarms in der Nähe von Buto, der durch den Vergleich der Medianwerte des NDWI zwischen Sommer- (Juli/August) und Wintersaison (Januar/Februar) (ΔNDWI) deutlich zu erkennen ist. Der beobachtete Unterschied ist wahrscheinlich auf eine geringere Boden- und/oder Pflanzenfeuchtigkeit während des Sommers zurückzuführen, welche möglicherweise durch grobkörnige Ablagerungen im Untergrund bedingt wird. Ähnliche Anomalien wurden in der unmittelbaren Umgebung mehrerer pleistozäner Sandhügel (Geziras) und Siedlungshügel (Tells) des östlichen Nildeltas gefunden, was die Kartierungen der potentiellen oberflächennahen Fortsetzung ermöglichte. Weitere lineare und mäandrierende ΔNDWI Anomalien wurden im östlichen Nildelta in der unmittelbaren Umgebung der antiken Stätte von Bubastis (Tell Basta) sowie einige Kilometer nördlich der Stadt Zagazig gefunden. Diese Anomalien weisen vermutlich auf frühere Verläufe von Flussarmen des Nils in diesem Bereich des Deltas hin. KW - Nile Delta KW - paleogeography Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-230349 VL - 69 IS - 2 ER - TY - JOUR A1 - Kunz, Julius A1 - Kneisel, Christof T1 - Three‐dimensional investigation of an open‐ and a closed‐system Pingo in northwestern Canada JF - Permafrost and Periglacial Processes N2 - The present study presents three-dimensional investigations of a hydrostatic pingo in the Mackenzie Delta region and a hydraulic pingo in the Ogilvie Mountains and contributes to a better understanding about the internal structures of the two pingo types. A combined approach using quasi-three-dimensional electrical resistivity tomography, ground-penetrating radar and frost probing allowed a clear delineation of frozen and unfrozen areas in the subsurface. At the hydrostatic pingo a massive ice core as well as a surrounding talik could be detected, but the location of the ice core and the talik differs from previous published assumptions. In contrast to acknowledged theory, at our site the massive ice core is not located in the center of the pingo but at the western edge, whereas the eastern flank is underlain by a talik, which surrounds the massive ice core. At the hydraulic pingo, the expected internal structure could be confirmed and the pathway of upwelling water could also be detected. The combined approach of the applied methods represents the first known three-dimensional geoelectrical investigation of pingos and provides new insights into the internal structure and architecture of the two different pingo types. The chosen approach allows further conclusions on the formation of these permafrost-affected landforms. KW - near surface multidimensional geophysics KW - pingos KW - permafrost hydrology KW - permafrost Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-257678 VL - 32 IS - 4 ER - TY - JOUR A1 - Schwalb‐Willmann, Jakob A1 - Remelgado, Ruben A1 - Safi, Kamran A1 - Wegmann, Martin T1 - moveVis: Animating movement trajectories in synchronicity with static or temporally dynamic environmental data in R JF - Methods in Ecology and Evolution N2 - Visualizing movement data is challenging: While traditional spatial data can be sufficiently displayed as two‐dimensional plots or maps, movement trajectories require the representation of time in a third dimension. To address this, we present moveVis, an R package, which provides tools to animate movement trajectories, overlaying simultaneous uni‐ or multi‐temporal raster imagery or vector data. moveVis automates the processing of movement and environmental data to turn such into an animation. This includes (a) the regularization of movement trajectories enforcing uniform time instances and intervals across all trajectories, (b) the frame‐wise mapping of movement trajectories onto temporally static or dynamic environmental layers, (c) the addition of customizations, for example, map elements or colour scales and (d) the rendering of frames into an animation encoded as GIF or video file. moveVis is designed to display interactions and concurrencies of animal movement and environmental data. We present examples and use cases, ranging from data exploration to visualizing scientific findings. Static spatial plots of movement data disregard the temporal dimension that distinguishes movement from other spatial data. In contrast, animations allow to display relocation in both time and space. We deem animations a powerful way to visually explore movement data, frame analytical findings and display potential interactions with spatially continuous and temporally dynamic environmental covariates. KW - animal tracking KW - animation KW - data visualization KW - movement data KW - movement ecology KW - spatio‐temporal data Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-214856 VL - 11 IS - 5 SP - 664 EP - 669 ER - TY - JOUR A1 - Stanley, Jean-Daniel A1 - Ullmann, Tobias A1 - Lange-Athinodorou, Eva T1 - Holocene aridity-induced interruptions of human activity along a fluvial channel in Egypt's northern delta JF - Quaternary N2 - Geoarchaeological information presented here pertains to a subsidiary Nile channel that once flowed west of the main Sebennitic distributary and discharged its water and sediments at Egypt’s then north-central deltaic coast. Periodical paleoclimatic episodes during the later Middle and Upper Holocene included decreased rainfall and increased aridity that reduced the Nile’s flow levels and thus likely disrupted nautical transport and anthropogenic activity along this channel. Such changes in this deltaic sector, positioned adjacent to the Levantine Basin in the Eastern Mediterranean, can be attributed to climatic shifts triggered as far as the North Atlantic to the west, and African highland source areas of the Egyptian Nile to the south. Of special interest in a study core recovered along the channel are several sediment sequences without anthropogenic material that are interbedded between strata comprising numerous potsherds. The former are interpreted here as markers of increased regional aridity and reduced Nile flow which could have periodically disrupted the regional distribution of goods and nautical activities. Such times occurred ~5000 years B.P., ~4200–4000 years B.P., ~3200–2800 years B.P., ~2300–2200 years B.P., and more recently. Periods comparable to these are also identified by altered proportions of pollen, isotopic and compositional components in different radiocarbon-dated Holocene cores recovered elsewhere in the Nile delta, the Levantine region to the east and north of Egypt, and in the Faiyum depression south of the delta. KW - Nile delta KW - Sebennitic KW - paleoenvironment KW - paleoclimate KW - Nile flow KW - geoarchaeology Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-250285 SN - 2571-550X VL - 4 IS - 4 ER - TY - JOUR A1 - Remelgado, Ruben A1 - Leutner, Benjamin A1 - Safi, Kamran A1 - Sonnenschein, Ruth A1 - Kuebert, Carina A1 - Wegmann, Martin T1 - Linking animal movement and remote sensing - mapping resource suitability from a remote sensing perspective JF - Remote Sensing in Ecology and Conservation N2 - Optical remote sensing is an important tool in the study of animal behavior providing ecologists with the means to understand species-environment interactions in combination with animal movement data. However, differences in spatial and temporal resolution between movement and remote sensing data limit their direct assimilation. In this context, we built a data-driven framework to map resource suitability that addresses these differences as well as the limitations of satellite imagery. It combines seasonal composites of multiyear surface reflectances and optimized presence and absence samples acquired with animal movement data within a cross-validation modeling scheme. Moreover, it responds to dynamic, site-specific environmental conditions making it applicable to contrasting landscapes. We tested this framework using five populations of White Storks (Ciconia ciconia) to model resource suitability related to foraging achieving accuracies from 0.40 to 0.94 for presences and 0.66 to 0.93 for absences. These results were influenced by the temporal composition of the seasonal reflectances indicated by the lower accuracies associated with higher day differences in relation to the target dates. Additionally, population differences in resource selection influenced our results marked by the negative relationship between the model accuracies and the variability of the surface reflectances associated with the presence samples. Our modeling approach spatially splits presences between training and validation. As a result, when these represent different and unique resources, we face a negative bias during validation. Despite these inaccuracies, our framework offers an important basis to analyze species-environment interactions. As it standardizes site-dependent behavioral and environmental characteristics, it can be used in the comparison of intra- and interspecies environmental requirements and improves the analysis of resource selection along migratory paths. Moreover, due to its sensitivity to differences in resource selection, our approach can contribute toward a better understanding of species requirements. KW - Landsat KW - movement ecology KW - optical remote sensing KW - resource mapping KW - resource suitability KW - surface reflectances Y1 - 2018 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-225199 VL - 4 IS - 3 ER - TY - JOUR A1 - Paeth, Heiko A1 - Pollinger, Felix T1 - Changes in mean flow and atmospheric wave activity in the North Atlantic sector JF - Quarterly Journal of the Royal Meteorological Society N2 - In recent years, the midlatitudes are characterized by more intense heatwaves in summer and sometimes severe cold spells in winter that might emanate from changes in atmospheric circulation, including synoptic‐scale and planetary wave activity in the midlatitudes. In this study, we investigate the heat and momentum exchange between the mean flow and atmospheric waves in the North Atlantic sector and adjacent continents by means of the physically consistent Eliassen–Palm flux diagnostics applied to reanalysis and forced climate model data. In the long‐term mean, momentum is transferred from the mean flow to atmospheric waves in the northwest Atlantic region, where cyclogenesis prevails. Further downstream over Europe, eddy fluxes return momentum to the mean flow, sustaining the jet stream against friction. A global climate model is able to reproduce this pattern with high accuracy. Atmospheric variability related to atmospheric wave activity is much more expressed at the intraseasonal rather than the interannual time‐scale. Over the last 40 years, reanalyses reveal a northward shift of the jet stream and a weakening of intraseasonal weather variability related to synoptic‐scale and planetary wave activity. This pertains to the winter and summer seasons, especially over central Europe, and correlates with changes in the North Atlantic Oscillation as well as regional temperature and precipitation. A very similar phenomenon is found in a climate model simulation with business‐as‐usual scenario, suggesting an anthropogenic trigger in the weakening of intraseasonal weather variability in the midlatitudes. KW - atmospheric waves KW - climate change KW - Elissen-Palm flux KW - jet stream Y1 - 2019 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-208079 VL - 145 IS - 725 ER - TY - JOUR A1 - Trappe, Julian A1 - Büdel, Christian A1 - Meister, Julia A1 - Baumhauer, Roland T1 - Combining geophysical and geomorphological data to reconstruct the development of relief of a medieval castle site in the Spessart low mountain range, Germany JF - Earth Surface Processes and Landforms N2 - Within the Spessart low mountain range in central Germany, numerous castle ruins of the 13th century ce exist. Their construction and destruction were often determined by the struggle for political and economic supremacy in the region and for control over the Spessart's natural resources. Wahlmich Castle is located in a relatively uncommon strategic and geomorphological position, characterized by a fairly remote position and atypical rough relief. In order to reconstruct the local relief development and possible human impact, a multi-method approach was applied combining two-dimensional geoelectrical measurements, geomorphological mapping and stratigraphic-sedimentological investigations. This provides new insights into the influence of landscape characteristics on choices of castle locations. The combined geoelectrical, geomorphological and stratigraphic-sedimentological data show that the rough relief is of natural origin and influenced by regional faulting, which triggered sliding and slumping as well as weathering and dissection of the surface deposits. The rough relief and the lithology permitted intensive land use and building activities. However, the location of the castle offered access to and possibly control over important medieval traffic routes and also represented certain ownership claims in the Aschaff River valley. The economic situation combined with rivalry between different elites led to the castle being built in a geomorphological challenging and strategically less valuable location. Focusing on castles located in rare and challenging geomorphological positions may therefore lead to a better understanding of castle siting in the future. KW - faulting KW - sedimentology KW - percussion core probing KW - geophysical prospection KW - geomorphological mapping KW - geoarchaeology Y1 - 2022 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-257433 VL - 47 IS - 1 ER - TY - JOUR A1 - Geyer, Gerd A1 - Pais, Miguel Caldeira A1 - Wotte, Thomas T1 - Unexpectedly curved spines in a Cambrian trilobite: considerations on the spinosity in Kingaspidoides spinirecurvatus sp. nov. from the Anti-Atlas, Morocco, and related Cambrian ellipsocephaloids JF - PalZ N2 - The new ellipsocephaloid trilobite species Kingaspidoides spinirecurvatus has a spectacular morphology because of a unique set of two long and anteriorly recurved spines on the occipital ring and the axial ring of thoracic segment 8. Together with the long genal spines this whimsical dorsally directed spine arrangement is thought to act as a non-standard protective device against predators. This is illustrated by the body posture during different stages of enrolment, contrasting with the more sophisticated spinosities seen in later trilobites, which are discussed in brief. Kingaspidoides spinirecurvatus from the lower–middle Cambrian boundary interval of the eastern Anti-Atlas in Morocco has been known for about two decades, with specimens handled as precious objects on the fossil market. Similar, but far less spectacular, spine arrangements on the thoracic axial rings are known from other ellipsocephaloid trilobites from the Anti-Atlas of Morocco and the Franconian Forest region of Germany. This suggests that an experimental phase of spine development took place within the Kingaspi-doides clade during the early–middle Cambrian boundary interval. KW - Cambrian KW - Trilobita KW - Systematics KW - Biostratigraphy KW - West Gondwana KW - Morocco Y1 - 2020 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-231873 SN - 0031-0220 VL - 94 ER - TY - JOUR A1 - Ibebuchi, Chibuike Chiedozie T1 - On the Relationship between Circulation Patterns, the Southern Annular Mode, and Rainfall Variability in Western Cape JF - Atmosphere N2 - This study investigates circulation types (CTs) in Africa, south of the equator, that are related to wet and dry conditions in the Western Cape, the statistical relationship between the selected CTs and the Southern Annular Mode (SAM), and changes in the frequency of occurrence of the CTs related to the SAM under the ssp585 scenario. Obliquely rotated principal component analysis applied to sea level pressure (SLP) was used to classify CTs in Africa, south of the equator. Three CTs were found to have a high probability of being associated with wet days in the Western Cape, and four CTs were equally found to have a high probability of being associated with dry days in the Western Cape. Generally, the dry/wet CTs feature the southward/northward track of the mid-latitude cyclone, adjacent to South Africa; anti-cyclonic/cyclonic relative vorticity, and poleward/equatorward track of westerlies, south of South Africa. One of the selected wet CTs was significantly related to variations of the SAM. Years with an above-average SAM index correlated with the below-average frequency of occurrences of the wet CT. The results suggest that through the dynamics of the CT, the SAM might control the rainfall variability of the Western Cape. Under the ssp585 scenario, the analyzed climate models indicated a possible decrease in the frequency of occurrence of the aforementioned wet CT associated with cyclonic activity in the mid-latitudes, and an increase in the frequency of the occurrence of CT associated with enhanced SLP at mid-latitudes. KW - Western Cape KW - Southern Annular Mode KW - circulation type KW - Africa south of the equator KW - mid-latitude cyclone Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-241018 SN - 2073-4433 VL - 12 IS - 6 ER -