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A Physics Based on Statistics Algorithm for Retrieving Land Surface Temperature and Soil Moisture From AMSR-E Passive Microwave Data

机译:基于统计算法的物理学从AMSR-E被动微波数据中提取地表温度和土壤水分

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A regression analysis between brightness of all AMSR bands and MODIS land surface temperature product provided by NASA indicated the 89VGHZ is the best single band to retrieve land surface temperature. According to simulation analysis of AIEM, we propose an algorithm for retrieving land surface temperature from AMSR-E data. The analysis results (more 800,000 pixel data set) indicate that the radiation mechanism of surface covered snow is different from others. In order to retrieve land surface temperature more accurately, the land surface at least are classified into two groups: non-snow covered land surface and snow covered land surface. In order to improve the practical and accuracy of the algorithm, we build different equation for different range of temperature. The average land surface temperature error is about 2-3℃ relative to the MODIS LST product. On the other hand, the emissivity of passive microwave is very important parameter for retrieving soil moisture. We compute the emissivty through land surface temperature. After analyzing the relationship between the emssivity and soil moisture by utilizing the simulation data of AIEM, we propose a method to retrieve the soil moisture and the preliminary analysis indicate that this method is available which partly eliminate the influence of roughness.
机译:NASA提供的所有AMSR波段的亮度与MODIS地表温度乘积之间的回归分析表明,89VGHZ是获取地表温度的最佳单波段。通过对AIEM的仿真分析,提出了一种从AMSR-E数据中提取地表温度的算法。分析结果(更多的800,000像素数据集)表明,表层积雪的辐射机制与其他机制不同。为了更准确地获取地表温度,至少将地表分为两类:非积雪地表和积雪地表。为了提高算法的实用性和准确性,我们针对不同的温度范围建立了不同的方程。相对于MODIS LST产品,平均地面温度误差约为2-3℃。另一方面,无源微波的发射率是获取土壤水分的重要参数。我们通过地面温度来计算发射率。通过利用AIEM的模拟数据分析了地表水与土壤水分之间的关​​系,提出了一种土壤水分的反演方法,初步分析表明该方法是可行的,部分消除了粗糙度的影响。

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