Actual evapotranspiration in drylands from in-situ and satellite data: assessing biophysical constraints
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Actual evapotranspiration in drylands from in-situ and satellite data : assessing biophysical constraints. / Garcia Garcia, Monica; Sandholt, Inge; Ceccato, Pietro; Ridler, Marc-Etienne Francois; Mougin, Eric ; Kergoat, Laurent; Morillas, Laura; Timouck, Franck; Fensholt, Rasmus; Domingo, Francisco .
I: Remote Sensing of Environment, Bind 131, 2013, s. 103-118.Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt
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TY - JOUR
T1 - Actual evapotranspiration in drylands from in-situ and satellite data
T2 - assessing biophysical constraints
AU - Garcia Garcia, Monica
AU - Sandholt, Inge
AU - Ceccato, Pietro
AU - Ridler, Marc-Etienne Francois
AU - Mougin, Eric
AU - Kergoat, Laurent
AU - Morillas, Laura
AU - Timouck, Franck
AU - Fensholt, Rasmus
AU - Domingo, Francisco
PY - 2013
Y1 - 2013
N2 - Improving regional estimates of actual evapotranspiration (¿¿) in water-limited regions located at climatic transition zones is critical. This study assesses an ¿¿ model (PT-JPL model) based on downscaling potential evapotranspiration according to multiple stresses at daily time-scale in two of these regions using MSG–SEVIRI (surface temperature and albedo) and MODIS products (NDVI, LAI and fPAR). An open woody savanna in the Sahel (Mali) and a Mediterranean grassland (Spain) were selected as test sites with Eddy Covariance data used for evaluation. The PT-JPL model was modified to run at a daily time step and the outputs from eight algorithms differing in the input variables and also in the formulation of the biophysical constraints (stresses) were compared with the ¿¿ from the Eddy Covariance. Model outputs were also compared with other modeling studies at similar global dryland ecosystems.The novelty of this paper is the computation of a key model parameter, the soil moisture constraint, relying on the concept of apparent thermal inertia (fSM-ATI) computed with surface temperature and albedo observations. Our results showed that fSM-ATI from both in-situ and satellite data produced satisfactory results for ¿¿ at the Sahelian savanna, comparable to parameterizations using field-measured Soil Water Content (SWC) with r2 greater than 0.80. In the Mediterranean grasslands however, with much lower daily ¿E values, model results were not as good as in the Sahel (r2 = 0.57–0.31) but still better than reported values from more complex models applied at the site such as the Two Source Model (TSM) or the Penman–Monteith Leuning model (PML).PT-JPL-daily model with a soil moisture constraint based on apparent thermal inertia, fSM-ATI offers great potential for regionalization as no field-calibrations are required and water vapor deficit estimates, required in the original version, are not necessary, being air temperature and the available energy (Rn-G) the only input variables required, apart from routinely available satellite products
AB - Improving regional estimates of actual evapotranspiration (¿¿) in water-limited regions located at climatic transition zones is critical. This study assesses an ¿¿ model (PT-JPL model) based on downscaling potential evapotranspiration according to multiple stresses at daily time-scale in two of these regions using MSG–SEVIRI (surface temperature and albedo) and MODIS products (NDVI, LAI and fPAR). An open woody savanna in the Sahel (Mali) and a Mediterranean grassland (Spain) were selected as test sites with Eddy Covariance data used for evaluation. The PT-JPL model was modified to run at a daily time step and the outputs from eight algorithms differing in the input variables and also in the formulation of the biophysical constraints (stresses) were compared with the ¿¿ from the Eddy Covariance. Model outputs were also compared with other modeling studies at similar global dryland ecosystems.The novelty of this paper is the computation of a key model parameter, the soil moisture constraint, relying on the concept of apparent thermal inertia (fSM-ATI) computed with surface temperature and albedo observations. Our results showed that fSM-ATI from both in-situ and satellite data produced satisfactory results for ¿¿ at the Sahelian savanna, comparable to parameterizations using field-measured Soil Water Content (SWC) with r2 greater than 0.80. In the Mediterranean grasslands however, with much lower daily ¿E values, model results were not as good as in the Sahel (r2 = 0.57–0.31) but still better than reported values from more complex models applied at the site such as the Two Source Model (TSM) or the Penman–Monteith Leuning model (PML).PT-JPL-daily model with a soil moisture constraint based on apparent thermal inertia, fSM-ATI offers great potential for regionalization as no field-calibrations are required and water vapor deficit estimates, required in the original version, are not necessary, being air temperature and the available energy (Rn-G) the only input variables required, apart from routinely available satellite products
U2 - 10.1016/j.rse.2012.12.016
DO - 10.1016/j.rse.2012.12.016
M3 - Journal article
VL - 131
SP - 103
EP - 118
JO - Remote Sensing of Environment
JF - Remote Sensing of Environment
SN - 0034-4257
ER -
ID: 45746194