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scarce, both spatially and temporally. Regional to global soil moisture data rely largely on simulation with land surface models (LSM) forced by meteorological data ( Srinivasan et al. 2000 ; Dirmeyer et al. 2002 ) or on satellite observations of active or passive microwaves in the L- to X-band range (1.4–11 GHz) such as those currently available from the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E; Jackson 1993 ; Njoku and Entekhabi 1996 ; Wagner et al. 1999 ; Owe
scarce, both spatially and temporally. Regional to global soil moisture data rely largely on simulation with land surface models (LSM) forced by meteorological data ( Srinivasan et al. 2000 ; Dirmeyer et al. 2002 ) or on satellite observations of active or passive microwaves in the L- to X-band range (1.4–11 GHz) such as those currently available from the Advanced Microwave Scanning Radiometer for Earth Observing System (AMSR-E; Jackson 1993 ; Njoku and Entekhabi 1996 ; Wagner et al. 1999 ; Owe
Powers J. G. , 2005 : A description of the advanced research WRF version 2 . NCAR Tech. Note NCAR/TN-468+STR, 88 pp . Staelin, D. H. , 1976 : Remote sensing of the atmospheric water vapor and liquid water with Nimbus-5 microwave spectrometer . J. Appl. Meteor. , 15 , 1204 – 1215 . Staelin, D. H. , and Chen F. W. , 2000 : Precipitation observations near 54 and 183 GHz using the NOAA-15 satellite . IEEE Trans. Geosci. Remote Sens. , 38 , 2322 – 2332 . Tartaglione, N. , Lanciani
Powers J. G. , 2005 : A description of the advanced research WRF version 2 . NCAR Tech. Note NCAR/TN-468+STR, 88 pp . Staelin, D. H. , 1976 : Remote sensing of the atmospheric water vapor and liquid water with Nimbus-5 microwave spectrometer . J. Appl. Meteor. , 15 , 1204 – 1215 . Staelin, D. H. , and Chen F. W. , 2000 : Precipitation observations near 54 and 183 GHz using the NOAA-15 satellite . IEEE Trans. Geosci. Remote Sens. , 38 , 2322 – 2332 . Tartaglione, N. , Lanciani
