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

机译:雪覆盖土壤反散射和排放的多层模型模拟

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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:本文将介绍通过使用主动和无源微波传感器的实验和理论研究的实验和理论研究概述。特别地,通过基于致密介质辐射转移(DMRT)的模型模拟研究了积雪的多层结构及其时间演化对反向散射和发射的影响。已经使用2007年至2011年在位于意大利阿尔卑斯山的东部的测试区域和2011年的冬季中收集的X场Cosmo涉及和多频微波辐射测量数据和多频微波辐射测量数据进行验证。雪参数。通过比较DMRT-QCA模型的多层版本进行的实验数据和模型模拟,分析了X-,KU和KA和KA频段在X-,KU和KA频段发射的微波反向散射的影响。该研究一直专注于典型的高山地区的积雪结构的影响。已经观察到,多层模型通常能够考虑复杂地层的效果,再现测量的反向散射和具有比单层较高的精度更高的光散。

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