Two-year global simulation of L-band brightness temperatures over land

被引:103
作者
Pellarin, T [1 ]
Wigneron, JP
Calvet, JC
Berger, M
Douville, H
Ferrazzoli, P
Kerr, YH
Lopez-Baeza, E
Pulliainen, J
Simmonds, LP
Waldteufel, P
机构
[1] CNRM, Meteo France, F-31057 Toulouse 1, France
[2] INRA, F-33883 Villenave Dornon, France
[3] ESA, Estec, Land Surfaces Unit, NL-2200 AG Noordwijk, Netherlands
[4] Univ Roma Tor Vergata, I-00133 Rome, Italy
[5] CESBIO, F-31401 Toulouse 4, France
[6] Univ Valencia, Fac Fis, E-46100 Valencia, Spain
[7] Helsinki Univ Technol, LST, FIN-02015 Helsinki, Finland
[8] Univ Reading, Reading RG6 6DW, Berks, England
[9] Serv Aeron, F-91371 Verrieres Le Buisson, France
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2003年 / 41卷 / 09期
关键词
global scale; L-band radiometry; modeling; soil moisture;
D O I
10.1109/TGRS.2003.815417
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
This letter presents a synthetic L-band (1.4 GHz) multiangular brightness temperature dataset over land surfaces that was simulated at a half-degree resolution and at the global scale. The microwave emission of various land-covers (herbaceous and woody vegetation, frozen and unfrozen bare soil, snow, etc.) was computed using a simple model [L-band Microwave Emission of the Biosphere (L-MEB)] based on radiative transfer equations. The soil and vegetation characteristics needed to initialize the L-MEB model were derived from existing land-cover maps. Continuous simulations from a land-surface scheme for 1987 and 1988 provided time series of the main variables driving the L-MEB model: soil temperature at the surface and at depth, surface soil moisture, proportion of frozen surface soil moisture, and snow cover characteristics. The obtained global maps constitute a useful dataset for a first evaluation of the sensitivity of future satellite-based L-band radiometry data to soil moisture.
引用
收藏
页码:2135 / 2139
页数:5
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