期刊
HYDROLOGY AND EARTH SYSTEM SCIENCES
卷 18, 期 3, 页码 1165-1188出版社
COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/hess-18-1165-2014
关键词
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资金
- French space agency (Centre National d'Etudes Spaciales, CNES) for the MiSTIGRI (MicroSatellite for Thermal Infrared Ground surface Imaging)
- FORMOSAT acquisition
- MISTRALS (Mediterranean Integrated STudies at Regional And Local Scales) SICMed (Continental Surfaces and Interfaces in the Mediterranean area) program
- European FP7 SIRIUS
- PLEIADES (Participatory multi-Level EO-assisted tools for Irrigation water management and Agricultural Decision-Support)
- IRD (Institut de Recherche pour le Developpement)
- ITSON (Instituto Tecnologico de SONora)
- University of Sonora
- Cadi Ayyad University (Morocco) in the setting up of the Yaqui experiment
Instantaneous evapotranspiration rates and surface water stress levels can be deduced from remotely sensed surface temperature data through the surface energy budget. Two families of methods can be defined: the contextual methods, where stress levels are scaled on a given image between hot/dry and cool/wet pixels for a particular vegetation cover, and single-pixel methods, which evaluate latent heat as the residual of the surface energy balance for one pixel independently from the others. Four models, two contextual (S-SEBI and a modified triangle method, named VIT) and two single-pixel (TSEB, SEBS) are applied over one growing season (December-May) for a 4 km x 4 km irrigated agricultural area in the semi-arid northern Mexico. Their performance, both at local and spatial standpoints, are compared relatively to energy balance data acquired at seven locations within the area, as well as an uncalibrated soilvegetation-atmosphere transfer (SVAT) model forced with local in situ data including observed irrigation and rainfall amounts. Stress levels are not always well retrieved by most models, but S-SEBI as well as TSEB, although slightly biased, show good performance. The drop in model performance is observed for all models when vegetation is senescent, mostly due to a poor partitioning both between turbulent fluxes and between the soil/plant components of the latent heat flux and the available energy. As expected, contextual methods perform well when contrasted soil moisture and vegetation conditions are encountered in the same image (therefore, especially in spring and early summer) while they tend to exaggerate the spread in water status in more homogeneous conditions (especially in winter). Surface energy balance models run with available remotely sensed products prove to be nearly as accurate as the uncalibrated SVAT model forced with in situ data.
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