Soil moisture, the hydrologic interface between surface and ground waters

被引：0
|
作者：
Engman, ET
机构：
来源：
REMOTE SENSING AND GEOGRAPHIC INFORMATION SYSTEMS FOR DESIGN AND OPERATION OF WATER RESOURCES SYSTEMS | 1997年 / 242期
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D O I：
暂无
中图分类号：
TP7 [遥感技术];
学科分类号：
081102 ; 0816 ; 081602 ; 083002 ; 1404 ;
摘要：
A hypothesis is presented that many hydrologic processes display a unique signature that is detectable with microwave remote sensing. These signatures are in the form of the spatial and temporal distributions of surface soil moisture. The specific hydrologic processes that may be detected include groundwater recharge and discharge zones, storm runoff contributing areas, regions of potential and less than potential evapotranspiration (ET), and information about the hydrologic properties of soils. In basin and hillslope hydrology, soil moisture is the interface between surface and ground waters.
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页码：129 / 140
页数：12
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