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Snow Crystal Orientation Effects on the Scattering of Passive Microwave Radiation

机译:雪晶取向对无源微波辐射散射的影响

摘要

For this study, consideration is given to the role crystal orientation plays in scattering and absorbing microwave radiation. A discrete dipole scattering model is used to measure the passive microwave radiation, at two polarizations (horizontal and vertical), scattered by snow crystals oriented in random and non random positions, having various sizes (ranging between 1 micrometers to 10,000 micrometers in radius), and shapes (including spheroids, cylinders, hexagons). The model results demonstrate that for the crystal sizes typically found in a snowpack, crystal orientation is insignificant compared to crystal size in terms of scattering microwave energy in the 8,100 gm (37 GHz) region of the spectrum. Therefore, the assumption used in radiative transfer approaches, where snow crystals are modeled as randomly oriented spheres, is adequate to account for the transfer of microwave energy emanating from the ground and passing through a snowpack.
机译:在这项研究中,考虑了晶体取向在散射和吸收微波辐射中的作用。离散偶极子散射模型用于测量两种极化(水平和垂直)的无源微波辐射,这些微波被定向在随机和非随机位置的雪晶散射,并具有各种尺寸(半径在1微米至10,000微米之间),和形状(包括球体,圆柱体,六边形)。模型结果表明,对于通常在积雪堆中发现的晶体尺寸,与晶体尺寸相比,在8100 gm(37 GHz)光谱范围内的散射微波能量方面,晶体取向微不足道。因此,在辐射传输方法中使用的假设(其中雪晶被建模为随机定向的球体)足以说明从地面发出并经过积雪的微波能量的转移。

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