Paper
1 August 1984 Microwave Remote Sensing Of Soil Moisture
Thomas J. Schmugge
Author Affiliations +
Proceedings Volume 0481, Recent Advances in Civil Space Remote Sensing; (1984) https://doi.org/10.1117/12.943093
Event: 1984 Technical Symposium East, 1984, Arlington, United States
Abstract
Because of the large contrast between the dielectric constant of liquid water and that of dry soil at microwave wavelength, there is a strong dependence of the thermal emission and radar backscatter from the soil on its moisture content. This dependence provides a means for the remote sensing of the moisture content in a surface layer approximately 5 cm thick. The feasibility of these techniques has been demonstrated from field, aircraft and spacecraft platforms. The soil texture, surface roughness, and vegetative cover affect the sensitivity of the microwave response to moisture variations with vegetation being the most important. It serves as an attenuating layer which can totally obscure the surface. Research has indicated that it is possible to obtain 5 or more levels of moisture discrimination and that a mature corn crop is the limiting vegetation situation.
© (1984) COPYRIGHT Society of Photo-Optical Instrumentation Engineers (SPIE). Downloading of the abstract is permitted for personal use only.
Thomas J. Schmugge "Microwave Remote Sensing Of Soil Moisture", Proc. SPIE 0481, Recent Advances in Civil Space Remote Sensing, (1 August 1984); https://doi.org/10.1117/12.943093
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Cited by 34 scholarly publications.
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KEYWORDS
Soil science

Microwave radiation

Dielectrics

Radiometry

Vegetation

Remote sensing

Backscatter

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