IGARSS '98. Sensing and Managing the Environment. 1998 IEEE International Geoscience and Remote Sensing. Symposium Proceedings. 1998
DOI: 10.1109/igarss.1998.702827
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Utilization of the first three Stokes parameters for the determination of precipitation characteristics

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“…In addition, the complexity and costs of polarimetric systems restrict our ability to obtain the measurements required to understand the variation of the polarimetric signatures associated with natural and artificial surfaces and targets as a function of the surface type, the state of the surface, and the environmental conditions. Using a passive or active polarimetric system it is possible to infer surface winds over ocean areas 1 , study the spatial scale of microwave brightness temperatures in boreal forests 2 , analyze precipitation characteristics 3 , and determine soil moisture 4 . This paper presents the polarimetric signatures of natural and artificial surfaces and targets measured using 35 and 94 GHz Direct Detection Polarimetric Radiometers (DDPR).…”
Section: Introductionmentioning
confidence: 99%
“…In addition, the complexity and costs of polarimetric systems restrict our ability to obtain the measurements required to understand the variation of the polarimetric signatures associated with natural and artificial surfaces and targets as a function of the surface type, the state of the surface, and the environmental conditions. Using a passive or active polarimetric system it is possible to infer surface winds over ocean areas 1 , study the spatial scale of microwave brightness temperatures in boreal forests 2 , analyze precipitation characteristics 3 , and determine soil moisture 4 . This paper presents the polarimetric signatures of natural and artificial surfaces and targets measured using 35 and 94 GHz Direct Detection Polarimetric Radiometers (DDPR).…”
Section: Introductionmentioning
confidence: 99%