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A simple methods for downscaling passive microwave based soil moisture
Merlin O., Chehbouni G., Walker J.P., Panciera R., Kerr Y.H.
IEEE Geoscience and Remote Sensing Letters 46 (2008) 786-796 - http://hal.ird.fr/ird-00390430
Articles dans des revues avec comité de lecture
Sciences du Vivant/Ecologie, Environnement/Ecosystèmes
A simple methods for downscaling passive microwave based soil moisture
O. Merlin ( ) 1, G. Chehbouni () 2, J.P. Walker 1, R. Panciera 1, Y.H. Kerr () 2
1 :  Department of Civil and Environmental Engineering (Melbourne)
http://www.ie.unimelb.edu.au/
University of Melbourne
Engineering Blocks , C & D The University of Melbourne Parkville 3010 VIC Australia
Australie
2 :  Centre d'études spatiales de la biosphère (CESBIO)
http://www.cesbio.ups-tlse.fr
CNRS : UMR5126 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
bpi 2801 18 Av Edouard Belin 31401 TOULOUSE CEDEX 4
France
This paper develops two alternative approaches for downscaling passive microwave-derived soil moisture. Ground and airborne data collected over the Walnut Gulch experimental watershed during the Monsoon'90 experiment were used to test these approaches. These data consisted of eight micrometeorological stations (METFLUX) and six flights of the L-band Push Broom Microwave Radiometer (PBMR). For each PBMR flight, the 180-m resolution L-band pixels covering the eight METFLUX sites were first aggregated to generate a 500-m “coarse-scale” passive microwave pixel. The coarse-scale-derived soil moisture was then downscaled to the 180-m resolution using two different surface soil moisture indexes (SMIs): 1) the evaporative fraction (EF), which is the ratio of the evapotranspiration to the total energy available at the surface; and 2) the actual EF (AEF), which is defined as the ratio of the actual-to-potential evapotranspiration. It is well known that both SMIs depend on the surface soil moisture. However, they are also influenced by other factors such as vegetation cover, soil type, root-zone soil moisture, and atmospheric conditions. In order to decouple the influence of soil moisture from the other factors, a land surface model was used to account for the heterogeneity of vegetation cover, soil type, and atmospheric conditions. The overall accuracy in the downscaled values was evaluated to 3% (vol.) for EF and 2% (vol.) for AEF under cloud-free conditions. These results illustrate the potential use of satellite-based estimates of instantaneous evapotranspiration on clear-sky days for downscaling the coarse-resolution passive microwave soil moisture.
Anglais

IEEE Geoscience and Remote Sensing Letters
Publisher Institute of Electrical and Electronics Engineers (IEEE)
ISSN 1545-598X 
non spécifiée
2008
46
786-796

Downscaling – evaporative fraction (EF) – evapotranspiration – passive microwave – surface soil moisture
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