Global-scale evaluation of roughness effects on C-Band AMSR-E observations
PARRENS, Marie
Interactions Sol Plante Atmosphère [UMR ISPA]
Centre d'études spatiales de la biosphère [CESBIO]
Interactions Sol Plante Atmosphère [UMR ISPA]
Centre d'études spatiales de la biosphère [CESBIO]
FERNÁNDEZ-MORÁN, Roberto
Interactions Sol Plante Atmosphère [UMR ISPA]
Universitat de València = University of Valencia [UV]
< Réduire
Interactions Sol Plante Atmosphère [UMR ISPA]
Universitat de València = University of Valencia [UV]
Langue
en
Article de revue
Ce document a été publié dans
Remote Sensing. 2015, vol. 7, n° 5, p. 5734-5757
MDPI
Résumé en anglais
Quantifying roughness effects on ground surface emissivity is an important step in obtaining high-quality soil moisture products from large-scale passive microwave sensors. In this study, we used a semi-empirical method ...Lire la suite >
Quantifying roughness effects on ground surface emissivity is an important step in obtaining high-quality soil moisture products from large-scale passive microwave sensors. In this study, we used a semi-empirical method to evaluate roughness effects (parameterized here by the parameter) on a global scale from AMSR-E (Advanced Microwave Scanning Radiometer for EOS) observations. AMSR-E brightness temperatures at 6.9 GHz obtained from January 2009 to September 2011, together with estimations of soil moisture from the SMOS (Soil Moisture and Ocean Salinity) L3 products and of soil temperature from ECMWF’s (European Centre for Medium-range Weather Forecasting) were used as inputs in a retrieval process. In the first step, we retrieved a parameter (referred to as the parameter) accounting for the combined effects of roughness and vegetation. Then, global MODIS NDVI data were used to decouple the effects of vegetation from those of surface roughness. Finally, global maps of the Hr parameters were produced and discussed. Initial results showed that some spatial patterns in the values could be associated with the main vegetation types (higher values of were retrieved generally in forested regions, intermediate values were obtained over crops and grasslands, and lower values were obtained over shrubs and desert) and topography. For instance, over the USA, lower values of were retrieved in relatively flat regions while relatively higher values were retrieved in hilly regions.< Réduire
Mots clés
soil moisture
Mots clés en anglais
soil surface roughness
AMSR-E
Origine
Importé de halUnités de recherche