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

K. Muzalevskiy, Z. Ruzicka
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Abstract

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.
用多频微波辐射观测测量温度分布——理论建模
本文提出了利用1.4 GHz、6.93 GHz、7.3 GHz和10.7 GHz频率的亮温观测测量北极冻土带表层土壤温度剖面的方法。利用美国阿拉斯加州北坡Toolik气候站实测的北极冻土带表层土壤的多频微波发射物理模型和介电模型,结合温度剖面,计算了亮温的“实测值”。在土壤温度分段线性剖面近似中,从亮度温度“实测值”中提取温度剖面,并与2010 - 2011年Toolik站实测温度剖面进行比较。0.6cm和16.0cm深度土壤温度反演值与实测值的均方根误差分别为1.3°C和3.2°C,决定系数分别为0.92和0.62。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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