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Influence of Vegetation Cover on the Oh Soil Moisture Retrieval Model: A Case Study of the Malinda Wetland, Tanzania

Influence of Vegetation Cover on the Oh Soil Moisture Retrieval Model: A Case Study of the Malinda Wetland, Tanzania

作     者:Fridah Kirimi David N. Kuria Frank Thonfeld Esther Amler Kenneth Mubea Salome Misana Gunter Menz Fridah Kirimi;David N. Kuria;Frank Thonfeld;Esther Amler;Kenneth Mubea;Salome Misana;Gunter Menz

作者机构:Department of Geography University of Bonn Bonn Germany Institute of Geomatics GIS & Remote Sensing Dedan Kimathi University of Technology Nyeri Kenya Department of Geography University of Dar es Salaam Dar es Salaam Tanzania 

出 版 物:《Advances in Remote Sensing》 (遥感技术进展(英文))

年 卷 期:2016年第5卷第1期

页      面:28-42页

学科分类:09[农学] 0903[农学-农业资源与环境] 090301[农学-土壤学] 

主  题:Surface Soil Moisture Oh Model Water Cloud Model Wetland TerraSAR-X 

摘      要:Soil moisture is an important parameter that drives agriculture, climate and hydrological systems. In addition, retrieval of soil moisture is important in the analysis as well as its influence on these systems. Radar imagery is best suited for this retrieval due to its all-weather capability and independence from solar irradiation. Soil moisture retrieval was done for the Malinda Wetland, Tanzania, during two time periods, March and September 2013. The aim of this paper was to analyze soil moisture retrieval performance when vegetation contribution is taken into account. Backscatter values were obtained from TerraSAR-X Spotlight mode imagery taken in March and September 2013. The backscatter values recorded by SAR imagery are influenced by vegetation, soil roughness and soil moisture. Thus, in order to obtain the backscatter due to soil moisture, the roughness and vegetation contribution are determined and decoupled from total backscatter. The roughness parameters were obtained from a Digital Surface Model (DSM) from Unmanned Aerial Vehicle (UAV) photographs whereas the vegetation parameter was obtained by inverting the Water Cloud Model (WCM). Lastly, soil moisture was retrieved using the Oh Model. The coefficient of correlation between the observed and retrieved was 0.39 for the month of March and 0.65 in the month of August. When the vegetation contribution was considered, the r2 for March was 0.64 and that in August was 0.74. The results revealed that accounting for vegetation improved soil moisture retrieval.

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