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首页> 外文期刊>Geoscience and Remote Sensing Letters, IEEE >Effects of Vertical Resolution in Plane-Parallel Atmospheric Model on Brightness Temperature
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Effects of Vertical Resolution in Plane-Parallel Atmospheric Model on Brightness Temperature

机译:平面平行大气模型中垂直分辨率对亮度温度的影响

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摘要

Currently, various radiative transfer (RT) schemes use their own number of layers in a plane-parallel atmospheric model to simulate the brightness temperature (TB) without considering the effect. The purpose of this letter is to understand numerically and analytically the TB uncertainty due to the layer number of the plane-parallel atmospheric model in RT schemes. Methodically, a plane-parallel atmospheric model in light rainfall and two RT schemes are used. The simulated TBs show a dependence on the number of layers in a plane-parallel atmosphere, which is due to the optical thickness. This letter suggests that the vertical resolution should be considered as a parameter in the forward model of RT schemes.
机译:当前,各种辐射传输(RT)方案在平行于平面的大气模型中使用它们自己的层数来模拟亮度温度(TB),而不考虑其影响。这封信的目的是从数值和分析上理解由于RT方案中平面平行大气模型的层数导致的TB不确定性。有条理地,使用了一个平面降雨大气模型和两个RT方案。模拟的TB显示出在平面平行气氛中对层数的依赖性,这归因于光学厚度。这封信建议在RT方案的正向模型中应将垂直分辨率视为一个参数。

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