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Identifying Smos and Smap Pixels that Exhibit Distinct Roughness-Vegetation Patterns in Level 2 Optical Thickness Retrievals

机译:识别在2级光学厚度检索中展现出不同粗糙度-植被模式的Smos和Smap像素

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The Soil Moisture Ocean Salinity (SMOS) and Soil Moisture Active Passive (SMAP) Level 2 Soil Moisture products both exhibit a dry bias over agricultural regions. In regions such as the U.S. Corn Belt, where vegetation water content is high during the growing season and near zero in the winter' the year can be split into periods where retrieved optical thickness is either representative of vegetation water content or surface roughness. We hypothesize that allowing roughness to vary with retrieved optical thickness outside of the growing season will improve the dry bias in the U.S. Corn Belt. Pixels that have a distinct boundary between rough soil and vegetated conditions need to be identified to determine where this modified retrieval process could be useful. SMOS auxiliary land surface fractions are used as a filter for forest, urban, and open water before visually inspecting timeseries of optical thickness for roughness-vegetation patterns.
机译:土壤水分海洋盐度(SMOS)和土壤水分主动-被动(SMAP)2级土壤水分产品在农业地区均表现出干燥偏见。在美国玉米带等地区,生长季节的植被含水量很高,而冬季则接近零,因此可以将这一年划分为几个阶段,在这段时间内所获得的光学厚度可以代表植被含水量或表面粗糙度。我们假设允许粗糙度随生长期以外光学厚度的变化而变化,这将改善美国玉米带的干偏。需要确定在粗糙土壤和植被条件之间有明显边界的像素,以确定这种修改后的检索过程在哪里有用。在目视检查光学厚度的时间序列中是否存在粗糙植被图案之前,SMOS辅助陆地表面部分用作森林,城市和开阔水域的过滤器。

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