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Soil Moisture Retrieval Using a Two-Dimensional L-Band Synthetic Aperture Radiometer in a Semiarid Environment

机译:在半干旱环境中使用二维L波段合成孔径辐射计反演土壤水分

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Surface soil moisture was retrieved from the L-band radiometer data collected in semiarid regions during the Soil Moisture Experiment in 2004. The 2-D synthetic aperture radiometer (2D-STAR) was flown over regional-scale study sites located in AZ, USA, and Sonora, Mexico (SO). The study sites are characterized by a range of topographic relief with a land cover that varies from bare soil to grass and scrubland and includes areas with high rock fraction near the soil surface. The 2D-STAR retrieval of soil moisture was in good agreement with the ground-based estimates of surface soil moisture in both AZ $(hbox{rmse} = 0.012 hbox{m}^{3} hbox{m}^{-3})$ and SO $(hbox{rmse} = 0.011 hbox{m}^{3} hbox{m}^{-3})$. The 2D-STAR also showed a good performance in the Walnut Gulch Experimental Watershed $(hbox{rmse} = 0.014 hbox{m}^{3} hbox{m}^{-3})$ where the surface soil featured high rock fraction was as high as 60%. Comparison of the results with the Polarimetric Scanning Radiometer at the C- and X-band data indicates the superior soil moisture retrieval performance of the L-band data over the regions with high rock fraction and moderate vegetation density.
机译:从2004年土壤水分实验期间在半干旱地区收集的L带辐射计数据中检索了表面土壤水分。将2D合成孔径辐射计(2D-STAR)送入了位于美国AZ,美国,和墨西哥索诺拉(SO)。研究地点的特点是一系列地形起伏,土地覆盖范围从裸露的土壤到草丛和灌丛,并包括靠近土壤表面的高岩石碎屑区域。在两个AZ $(hbox {rmse} = 0.012 hbox {m} ^ {3} hbox {m} ^ {-3}中,土壤水分的2D-STAR检索与地面土壤水分的地面估算值非常吻合。 )$和SO $(hbox {rmse} = 0.011 hbox {m} ^ {3} hbox {m} ^ {-3})$。 2D-STAR在核桃谷实验分水岭$(hbox {rmse} = 0.014 hbox {m} ^ {3} hbox {m} ^ {-3})$中也表现出良好的性能,其中表层土壤的岩石碎屑含量高高达60%在C波段和X波段数据上与极化扫描辐射计进行的结果比较表明,在岩石分数高,植被密度中等的地区,L波段数据的土壤水分反演性能优异。

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