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Development of Microwave Emission Model for Frozen Soil with Considering the Volume Scattering Effect

机译:考虑体积散射效应的冷冻土微波发射模型的开发

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Land surface freeze/thaw (F/T) has an important influence on the carbon cycle of the ecosystem, hydrological and meteorological. Affected by the frozen of water in soil, the frozen soil would become larger soil particles due to condensation, resulting in its soil particles being larger than those of the melting soil. The microwave radiation of frozen soil has a significant volume scattering effect in the high frequency band due to large particles of frozen soil. This paper developed a frozen soil microwave emission model considering the volume scattering effect of frozen soil particles based on dense media radiative transfer (DMRT) model [1] by combining experimental data and numerical simulation. The simulation results of the frozen soil microwave emission model, combined model for cold land [2] and the three-layer incoherent media model [3] were validated and compared with the experimental data. Results show that frozen soil microwave emission model which considering the volume scattering effect of frozen soil is better than the other two models. It is necessary to consider the volume scattering effect of frozen soil.
机译:土地表面冻融/解冻(F / T)对生态系统,水文和气象的碳循环具有重要影响。受土壤中水冻的影响,冻土将成为由于缩合而变大的土壤颗粒,导致其土壤颗粒大于熔化的土壤。由于大颗粒的冷冻土壤,冷冻土壤的微波辐射在高频带中具有显着的体积散射效果。本文通过结合实验数据和数值模拟,开发了一种冻土微波发射模型,考虑了冻土颗粒的体积散射效果(DMRT)模型[1]。冷冻土壤微波发射模型,冷陆综合模型及三层非连贯介质模型[3]的仿真结果验证并与实验数据进行了验证。结果表明,冻土微波发射模型,考虑冻土的体积散射效果优于其他两种型号。有必要考虑冷冻土壤的体积散射效果。

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