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Performance Of Sea Surface Salinity And Soil Moisture Retrieval Algorithms With Different Auxiliary Datasets In 2-D L-Band Aperture Synthesis Interferometric Radiometers

机译:二维L波段合成干涉辐射计中不同辅助数据集的海面盐度和土壤水分反演算法

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摘要

The Soil Moisture and Ocean Salinity (SMOS) Earth Explorer Opportunity Mission was selected in May 1999 by the European Space Agency Earth Observation Programme Board to provide global and frequent soil moisture (SM) and sea surface salinity (SSS) maps. SMOS' single payload is the Microwave Imaging Radiometer by Aperture Synthesis (MIRAS) sensor, an L-band two-dimensional aperture synthesis interferometric radiometer with multiangular and polarimetric imaging capabilities. The definition of the SMOS Level 2 Processor requires the selection of the optimum operation mode (dual-polarization or full-polarimetric) for each application, the specification of the required auxiliary data, and the optimum retrieval algorithms. Using the SMOS simulator and based on the experience gained in previous works, this paper presents a study of the SM and SSS retrieval capabilities over homogeneous pixels, in the two modes of operation with different auxiliary data. It is found that SSS retrievals using the first Stokes parameter measured in the dual-polarization mode perform somewhat worse than using the vertical (T/sub vv/) and horizontal (T/sub hh/) brightness temperatures measured in the full-polarimetric mode, and the performance degrades for cold waters due to the lower sensitivity of the brightness temperature to SSS at low sea surface temperature (SST). Due to the larger angular variation of T/sub hh/ and T/sub vv/, SM retrievals using T/sub hh/ and T/sub vv/ measured in the full-polarimetric mode exhibit a significant better performance over bare soils than over vegetation-covered soils. Over vegetation-covered soils vegetation parameters (opacity and albedo) can be inferred over a 550-km swath width in the full-polarimetric mode. However, since the first Stokes parameter is independent of both geometric and Faraday rotations, it is very robust in the presence of instrumental and geophysical errors. In the SSS retrieval problem and in the SM retrieval problem (with T/sub hh/ and T/sub vv/ measured in the full-polarimetric mode), the performance of the retrieval algorithms tested is not significantly altered if the model parameters are not exactly known, but are left as adjustable parameters in the optimization process.
机译:1999年5月,欧洲航天局地球观测计划委员会选择了土壤湿度和海洋盐度(SMOS)地球探索者机会任务,以提供全球和频繁的土壤湿度(SM)和海面盐度(SSS)地图。 SMOS的唯一有效载荷是孔径合成微波成像辐射仪(MIRAS)传感器,它是一种具有多角度和偏振成像功能的L波段二维孔径合成干涉辐射仪。 SMOS 2级处理器的定义要求针对每种应用选择最佳操作模式(双极化或全极化),所需辅助数据的规范以及最佳检索算法。本文使用SMOS模拟器并基于先前工作中获得的经验,对具有不同辅助数据的两种操作模式下均质像素上的SM和SSS检索能力进行了研究。发现使用在双极化模式下测量的第一个Stokes参数进行SSS检索比使用在全极化模式下测量的垂直(T / sub vv /)和水平(T / sub hh /)亮度温度要差一些,并且由于在低海面温度(SST)下亮度温度对SSS的敏感性较低,因此冷水的性能下降。由于T / sub hh /和T / sub vv /的较大角度变化,使用T / sub hh /和T / sub vv /在全极化模式下进行的SM反演在裸土上的性能要好于在裸土上植被覆盖的土壤。在植被覆盖的土壤上,可以在全极化模式下在550 km的条带宽度上推断出植被参数(不透明度和反照率)。但是,由于第一个斯托克斯参数与几何旋转和法拉第旋转均无关,因此在存在仪器和地球物理误差的情况下,它非常健壮。在SSS检索问题和SM检索问题中(在全极化模式下测量T / sub hh /和T / sub vv /),如果模型参数未设置,则测试的检索算法的性能不会显着改变确切已知,但在优化过程中保留为可调参数。

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