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A physics-based statistical algorithm for retrieving land surface temperature from AMSR-E passive microwave data

机译:一种基于物理的统计算法,用于从AMSR-E无源微波数据中检索地表温度

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摘要

AMSR-E and MODIS are two EOS (Earth Observing System) instruments on board the Aqua satellite. A regression analysis between the brightness of all AMSR-E bands and the MODIS land surface temperature product indicated that the 89 GHz vertical polarization is the best single band to retrieve land surface temperature. According to simulation analysis with AIEM, the difference of different frequencies can eliminate the influence of water in soil and atmosphere, and also the surface roughness partly. The analysis results 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 should be at least classified into three types: water covered surface, snow covered surface, and non-water and non-snow covered land surface. In order to improve the practicality and accuracy of the algorithm, we built different equations for different ranges of temperature. The average land surface temperature error is about 2—3℃ relative to the MODIS LST product.
机译:AMSR-E和MODIS是Aqua卫星上的两个EOS(地球观测系统)仪器。所有AMSR-E波段的亮度与MODIS地表温度乘积之间的回归分析表明,89 GHz垂直极化是获取地表温度的最佳单波段。根据AIEM的仿真分析,不同频率的差异可以消除水对土壤和大气的影响,并部分消除表面粗糙度。分析结果表明,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,应至少将地表分为三类:水覆盖地表,雪覆盖地表以及非水和非雪地表地。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℃。

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