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Multi-layer model simulations of backscattering and emission from snow covered soils

机译:积雪土壤反向散射和排放的多层模型模拟

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摘要

In this paper an overview of experimental and theoretical investigations concerning snow cover by using both active and passive microwave sensors will be presented. In particular, the effects of multi-layer structure of snowpack and its temporal evolution on backscattering and emission have been investigated by model simulations based on the Dense Medium Radiative Transfer (DMRT). The implemented model has been validated using both X- band Cosmo SkyMed acquisitions and multi-frequency microwave radiometric data collected in the winters between 2007 and 2011 on a test area located in the Eastern part of the Italian Alps, and corresponding direct measurements of the main snow parameters. The effect of snow parameters on microwave backscattering at X- band and emission at X-, Ku- and Ka-bands has been analyzed by comparing experimental data and model simulations performed with a multi-layer version of the DMRT-QCA model. The study has been focused on the effect of layering structure of snowpack typical of the Alpine regions. It has been observed that the multi-layer model is generally able to account for the effects of complex stratigraphy, reproducing the measured backscattering and emission with a higher accuracy than the single layer one.
机译:本文将概述使用主动和被动微波传感器进行的关于积雪的实验和理论研究的概况。特别是,通过基于密集介质辐射传输(DMRT)的模型模拟研究了积雪的多层结构及其时间演变对反向散射和排放的影响。已使用X波段Cosmo SkyMed采集数据和2007年至2011年冬季在意大利阿尔卑斯山东部地区的测试区域收集的多频微波辐射数据,以及相应的直接主测量数据,对所实施的模型进行了验证。雪参数。通过比较实验数据和使用多层版本DMRT-QCA模型进行的模型仿真,分析了雪参数对X波段微波反向散射和X波段,Ku波段和Ka波段发射的影响。该研究集中在高山地区典型积雪的分层结构的影响上。已经观察到,多层模型通常能够解决复杂地层的影响,以比单层模型更高的精度再现所测得的反向散射和发射。

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