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  - Saddique, Naeem
A1  - Usman, Muhammad
A1  - Bernhofer, Christian
T1  - Simulating the impact of climate change on the hydrological regimes of a sparsely gauged mountainous basin, northern Pakistan
JF  - Water
N2  - Projected climate changes for the 21st century may cause great uncertainties on the hydrology of a river basin. This study explored the impacts of climate change on the water balance and hydrological regime of the Jhelum River Basin using the Soil and Water Assessment Tool (SWAT). Two downscaling methods (SDSM, Statistical Downscaling Model and LARS-WG, Long Ashton Research Station Weather Generator), three Global Circulation Models (GCMs), and two representative concentration pathways (RCP4.5 and RCP8.5) for three future periods (2030s, 2050s, and 2090s) were used to assess the climate change impacts on flow regimes. The results exhibited that both downscaling methods suggested an increase in annual streamflow over the river basin. There is generally an increasing trend of winter and autumn discharge, whereas it is complicated for summer and spring to conclude if the trend is increasing or decreasing depending on the downscaling methods. Therefore, the uncertainty associated with the downscaling of climate simulation needs to consider, for the best estimate, the impact of climate change, with its uncertainty, on a particular basin. The study also resulted that water yield and evapotranspiration in the eastern part of the basin (sub-basins at high elevation) would be most affected by climate change. The outcomes of this study would be useful for providing guidance in water management and planning for the river basin under climate change.
KW  - water balance
KW  - hydrological regime
KW  - evapotranspiration
KW  - uncertainties
KW  - climate change
KW  - SWAT
Y1  - 2019
U6  - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:bvb:20-opus-193175
SN  - 2073-4441
VL  - 11
IS  - 10
ER  -