Publication | Closed Access
Microwave Backscatter Dependence on Surface Roughness, Soil Moisture, and Soil Texture: Part I-Bare Soil
504
Citations
4
References
1978
Year
Environmental MonitoringEngineeringPart I-bare SoilLand DegradationTerrestrial SensingEarth ScienceSoil CharacterizationSoil PropertyMicrowave Backscatter DependenceSoil MoistureActive Microwave RemoteMoisture ContentSynthetic Aperture RadarAntennaMicrowave Remote SensingGeographyRadiation MeasurementMicrowave MeasurementRadiometryPrecision Soil MappingRadar ImagingRadarRadar ScatteringRemote Sensing
This study is the first of a two‑part series using active microwave remote sensing to measure moisture in bare and vegetated soils. The study aims to evaluate how backscatter varies with soil moisture to inform radar system design for future airborne or spaceborne soil‑moisture mapping. The authors conducted an experimental program measuring backscatter across varying soil moisture, surface roughness, and texture, focusing on roughness effects and preliminarily assessing texture influence. Results confirm that operating near 5 GHz over 7–17° incidence reduces surface‑roughness effects, that surface‑soil moisture estimates match ground‑truth precision, and that the depth contributing to backscatter could not be experimentally isolated due to strong correlation with subsurface moisture.
This is the first in a series of two papers on the use of active microwave remote sensing for measuring the moisture content of bare (Part I) and vegetation-covered (Part II) soil. An experimental program was conducted to evaluate the response of the backscattering coefficient to soil moisture content as a means to specify radar system parameters for future airborne and/or spaceborne soil moisture mappers. Particular attention was paid to the effects of surface roughness, and a preliminary examination of the role of soil texture was performed. The results of this investigation confirm the findings of a previous experiment [1] which concluded that the effects of surface roughness can be minimized by operating at a frequency in the neighborhood of 5 GHz over the 7-17° angle of incidence range. The precision with which soil moisture in the surface soil layer can be estimated is comparable to the precision of the ground-truthed estimate. Because the moisture in the surface layer is highly correlated to the subsurface moisture, it was not possible to determine experimentally the effective depth of the layer responsible for the observed radar backscatter.
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