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Measuring temperature profile using multi-frequency microwave radiometric observation-theoretical modeling

机译:使用多频微波辐射观测理论模型测量温度剖面

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In this theoretical paper, we propose method for the measurement of temperature profile in the topsoil of Arctic tundra using observations of brightness temperature at frequencies of 1.4, 6.93, 7.3 and 10.7 GHz. A multi-frequency physical model of microwave emission of bare soil and dielectric model of Arctic tundra soil, with temperature profiles, which were measured in the active topsoil with using Toolik climate station on the North Slope of Alaska, were used to calculate “measured” values of brightness temperature. In the approximation of piecewise linear profile of soil temperature, from the “measured” values of brightness temperature were retrieved temperature profiles and were compared with ones, which were measured at the Toolik station from 2010 to 2011. The retrieved values of soil temperatures at the depth of 0.6cm and 16.0cm deviated from measured ones by 1.3°C and 3.2°C in terms of root-mean-square error, and by 0.92 and 0.62 in terms of determination coefficient, respectively.
机译:在该理论论文中,我们提出了使用观测温度为1.4、6.93、7.3和10.7 GHz的亮温来测量北极苔原表层土壤温度曲线的方法。使用阿拉斯加北坡的Toolik气候站在活动表层土壤中测量的裸露土壤微波发射的多频物理模型和北极苔原土壤的介电模型,以及温度分布图,用于计算“测量值”亮度温度值。在土壤温度的分段线性分布近似中,从“测得的”亮度温度值中检索出温度分布,并将其与在2010年至2011年在Toolik站测得的温度分布进行比较。 0.6厘米和16.0厘米的深度与均方根的均方根误差相差1.3°C和3.2°C,测定系数相差0.92和0.62。

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