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contributor authorJackson, Thomas J.
contributor authorHsu, Ann Y.
contributor authorO'Neill, Peggy E.
date accessioned2017-06-09T16:17:18Z
date available2017-06-09T16:17:18Z
date copyright2002/12/01
date issued2002
identifier issn1525-755X
identifier otherams-65060.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206243
description abstractStudies have shown the advantages of low-frequency (<5 GHz) microwave sensors for soil moisture estimation. Although higher frequencies have limited soil moisture retrieval capabilities, there is a vast quantity of systematic global high-frequency microwave data that have been collected for 15 yr by the Special Sensor Microwave Imager (SSM/I). SSM/I soil moisture studies have mostly utilized antecedent precipitation indices as validation, while only a few have employed limited ground observations, which were typically not optimal for this particular type of satellite data. In the Southern Great Plains (SGP) hydrology experiments conducted in 1997 and 1999, ground observations of soil moisture were made over an extended region for developing and validating large-scale mapping techniques. Previous studies have indicated the limitations of both the higher-frequency data and models for soil moisture retrieval. Given these limitations, an alternative retrieval technique that utilizes multipolarization observations was implemented and tested for the SGP region. A technique for extracting algorithm parameters from the observations was developed and tested. The algorithm was then used to produce soil moisture maps of the region for the two study periods.
publisherAmerican Meteorological Society
titleSurface Soil Moisture Retrieval and Mapping Using High-Frequency Microwave Satellite Observations in the Southern Great Plains
typeJournal Paper
journal volume3
journal issue6
journal titleJournal of Hydrometeorology
identifier doi10.1175/1525-7541(2002)003<0688:SSMRAM>2.0.CO;2
journal fristpage688
journal lastpage699
treeJournal of Hydrometeorology:;2002:;Volume( 003 ):;issue: 006
contenttypeFulltext


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