Merlin O., Chirouze Jonas, Olioso A., Jarlan Lionel, Chehbouni Abdelghani, Boulet Gilles. (2014). An image-based four-source surface energy balance model to estimate crop evapotranspiration from solar reflectance/thermal emission data (SEB-4S). Agricultural and Forest Meteorology, 184, p. 188-203. ISSN 0168-1923.
Titre du document
An image-based four-source surface energy balance model to estimate crop evapotranspiration from solar reflectance/thermal emission data (SEB-4S)
Agricultural and Forest Meteorology, 2014,
184, p. 188-203 ISSN 0168-1923
A remote sensing-based surface energy balance model is developed to explicitly represent the energy fluxes of four surface components of agricultural fields including bare soil, unstressed green vegetation, non-transpiring green vegetation, and standing senescent vegetation. Such a four-source representation (SEB-4S) is achieved by a consistent physical interpretation of the edges and vertices of the polygon (named T-f(vg) polygon) obtained by plotting surface temperature (T) as a function of fractional green vegetation (f(vg)) and the polygon (named T - alpha polygon) obtained by plotting T as a function of surface albedo (alpha). To test the performance of SEB-4S, a T-alpha image-based model and a T-f(vg) image-based model are implemented as benchmarks. The three models are tested over a 16 km by 10 km irrigated area in northwestern Mexico during the 2007-2008 agricultural season. Input data are composed of ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) thermal infrared, Formosat-2 shortwave, and station-based meteorological data. The fluxes simulated by SEB-4S, the T- alpha image-based model, and the T-f(vg) image-based model are compared on seven ASTER overpass dates with the in situ measurements collected at six locations within the study domain. The evapotranspiration simulated by SEB-4S is significantly more accurate and robust than that predicted by the models based on a single (either T-f(vg) or T- alpha) polygon. The improvement provided with SEB-4S reaches about 100W m(-2) at low values and about 100W m(-2) at the seasonal peak of evapotranspiration as compared with both the T- alpha and T-f(vg) image-based models. SEB-4S can be operationally applied to irrigated agricultural areas using high-resolution solar/thermal remote sensing data, and has potential to further integrate microwave-derived soil moisture as additional constraint on surface soil energy and water fluxes.
Plan de classement
Sciences fondamentales / Techniques d'analyse et de recherche [020]
;
Bioclimatologie [072]
;
Télédétection [126]
