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Retrieving Soil Moisture and temperature using SMOS observations at a test site in the Yamal Peninsular

机译:在亚马尔半岛的测试地点使用SMOS观测数据获取土壤水分和温度

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In this paper, the results of radiothermal remote sensing of soil moisture and temperature is presented for a test site located in Arctic tundra on the Yamal Peninsula, the Russia Federation using full-polarimetry multi-angular brightness temperature (BT) observations at the frequency of 1.4 GHz. The BT data were obtained from the Soil Moisture and Ocean Salinity (SMOS) satellite with the SMOS footprint near the polar weather station Marresale, Yamal Peninsular, the Russia Federation. The SMOS data covered the period of on the ground observations conducted in August, 2015. The method to retrieve soil moisture and temperature is based on solving an inverse problem by minimizing the norm of the residuals between the observed and predicted values of BTs. The calculation of BT was performed using semi-empirical model of radiothermal emission and temperature-dependent dielectric model for an organic-rich tundra soil. The obtained results revealed the applicability of the SMOS data for simultaneous retrieving the soil moisture and temperature for the Arctic tundra environment.
机译:在本文中,使用全极化多角度亮度温度(BT)观测资料,对位于俄罗斯联邦亚马尔半岛北极苔原上的一个测试地点的土壤湿度和温度进行了辐射热遥感的结果。 1.4 GHz。 BT数据是从土壤水分和海洋盐度(SMOS)卫星获得的,SMOS足迹位于俄罗斯联邦亚马尔半岛极地气象站Marresale附近。 SMOS数据涵盖了2015年8月进行的实地观测期。检索土壤水分和温度的方法是通过最小化BTs观测值与预测值之间的残差范数来解决反问题。使用富含有机物的冻原土壤的辐射热发射半经验模型和依赖温度的介电模型进行BT的计算。获得的结果表明,SMOS数据可用于同时获取北极苔原环境的土壤水分和温度。

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