TY - JOUR A1 - Timmermans, Wim J. A1 - van der Tol, Christiaan A1 - Timmermans, Joris A1 - Ucer, Murat A1 - Chen, Xuelong A1 - Alonso, Luis A1 - Moreno, Jose A1 - Carrara, Arnaud A1 - Lopez, Ramon A1 - Fernando de la Cruz, Tercero A1 - Corcoles, Horacio L. A1 - de Miguel, Eduardo A1 - Sanchez, Jose A. G. A1 - Perez, Irene A1 - Belen, Perez A1 - Munoz, Juan-Carlos J. A1 - Skokovic, Drazen A1 - Sobrino, Jose A1 - Soria, Guillem A1 - MacArthur, Alasdair A1 - Vescovo, Loris A1 - Reusen, Ils A1 - Andreu, Ana A1 - Burkart, Andreas A1 - Cilia, Chiara A1 - Contreras, Sergio A1 - Corbari, Chiara A1 - Calleja, Javier F. A1 - Guzinski, Radoslaw A1 - Hellmann, Christine A1 - Herrmann, Ittai A1 - Kerr, Gregoire A1 - Lazar, Adina-Laura A1 - Leutner, Benjamin A1 - Mendiguren, Gorka A1 - Nasilowska, Sylwia A1 - Nieto, Hector A1 - Pachego-Labrador, Javier A1 - Pulanekar, Survana A1 - Raj, Rahul A1 - Schikling, Anke A1 - Siegmann, Bastian A1 - von Bueren, Stefanie A1 - Su, Zhongbo (Bob) T1 - An Overview of the Regional Experiments for Land-atmosphere Exchanges 2012 (REFLEX 2012) Campaign JF - Acta Geophysica N2 - The REFLEX 2012 campaign was initiated as part of a training course on the organization of an airborne campaign to support advancement of the understanding of land-atmosphere interaction processes. This article describes the campaign, its objectives and observations, remote as well as in situ. The observations took place at the experimental Las Tiesas farm in an agricultural area in the south of Spain. During the period of ten days, measurements were made to capture the main processes controlling the local and regional land-atmosphere exchanges. Apart from multi-temporal, multi-directional and multi-spatial space-borne and airborne observations, measurements of the local meteorology, energy fluxes, soil temperature profiles, soil moisture profiles, surface temperature, canopy structure as well as leaf-level measurements were carried out. Additional thermo-dynamical monitoring took place at selected sites. After presenting the different types of measurements, some examples are given to illustrate the potential of the observations made. KW - multi scale heterogeneity KW - quantitative remote sensing KW - remote KW - evapotranspiration KW - validation KW - issues KW - energy KW - models KW - water KW - flux KW - land-atmosphere interaction KW - turbulence KW - calibration and validation Y1 - 2015 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-136491 VL - 63 IS - 6 ER - TY - JOUR A1 - Reiners, Philipp A1 - Asam, Sarah A1 - Frey, Corinne A1 - Holzwarth, Stefanie A1 - Bachmann, Martin A1 - Sobrino, Jose A1 - Göttsche, Frank-M. A1 - Bendix, Jörg A1 - Kuenzer, Claudia T1 - Validation of AVHRR Land Surface Temperature with MODIS and in situ LST — a TIMELINE thematic processor JF - Remote Sensing N2 - Land Surface Temperature (LST) is an important parameter for tracing the impact of changing climatic conditions on our environment. Describing the interface between long- and shortwave radiation fluxes, as well as between turbulent heat fluxes and the ground heat flux, LST plays a crucial role in the global heat balance. Satellite-derived LST is an indispensable tool for monitoring these changes consistently over large areas and for long time periods. Data from the AVHRR (Advanced Very High-Resolution Radiometer) sensors have been available since the early 1980s. In the TIMELINE project, LST is derived for the entire operating period of AVHRR sensors over Europe at a 1 km spatial resolution. In this study, we present the validation results for the TIMELINE AVHRR daytime LST. The validation approach consists of an assessment of the temporal consistency of the AVHRR LST time series, an inter-comparison between AVHRR LST and in situ LST, and a comparison of the AVHRR LST product with concurrent MODIS (Moderate Resolution Imaging Spectroradiometer) LST. The results indicate the successful derivation of stable LST time series from multi-decadal AVHRR data. The validation results were investigated regarding different LST, TCWV and VA, as well as land cover classes. The comparisons between the TIMELINE LST product and the reference datasets show seasonal and land cover-related patterns. The LST level was found to be the most determinative factor of the error. On average, an absolute deviation of the AVHRR LST by 1.83 K from in situ LST, as well as a difference of 2.34 K from the MODIS product, was observed. KW - Land Surface Temperature KW - AVHRR KW - MODIS KW - time series KW - Europe KW - validation KW - TIMELINE Y1 - 2021 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-246051 SN - 2072-4292 VL - 13 IS - 17 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 -