INVERSION OF SURFACE SOIL MOISTURE FROM RADAR ALTIMETRY BACKSCATTERING IN SEMI-ARID ENVIRONMENTS

被引：0
作者：
Blarel, Fabien [1 ]
Frappart, Frederic [1 ,2 ]
Mougin, Eric [2 ]
Ottle, Catherine [3 ]
Grippa, Manuela [2 ]
Ramillien, Guillaume [2 ]
Raoult, Nina [3 ]
机构：
[1] LEGOS OMP, Toulouse, France
[2] GET OMP, Toulouse, France
[3] LSCE, Gif Sur Yvette, France
来源：
IGARSS 2018 - 2018 IEEE INTERNATIONAL GEOSCIENCE AND REMOTE SENSING SYMPOSIUM | 2018年
关键词：
Soil moisture; backscattering; radar altimetry; ENVISAT;
D O I：
暂无
中图分类号：
TM [电工技术]; TN [电子技术、通信技术];
学科分类号：
0808 ; 0809 ;
摘要：
Surface Soil Moisture (SSM) is a key parameter of water and energy balances in semi-arid areas. SSM is linearly related to the radar backscattering coefficients (sigma(0)) over sand. Linear relationships are commonly used for inverting SSM in semi-arid areas from SAR and scatterometer data. Recent studies demonstrated that SSM can also be inversed from radar altimetry backscattering. An inversion method combining radar altimetry o-o and land surface model (LSM) outputs is proposed here.
引用
收藏
页码：9110 / 9113
页数：4
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