存在三维辐射效应时根据天底反射率对云光学厚度检索进行校正。第一部分:三维 RT 模拟的概念和测试

M. Alexandrov, Brian Cairns, C. Emde, B. van Diedenhoven
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引用次数: 0

摘要

在基于一维辐射传输计算(如广泛使用的双谱技术)的机载和卫星检索中,三维效应会导致云光学厚度(COT)被严重低估。对于单层孤立云,我们提出了一种简单的线性校正方法,其重归一化系数取决于云的纵横比(云的垂直和水平尺寸之比)。这是一个经验假设,我们使用合成的 3D RT 数据对其进行了成功测试。我们引入了三维辐射效应的启发式 "块模型",并证明重正化因子的函数形式与基本三维几何中云侧的辐射逃逸过程是一致的。我们还将块模型扩展到相邻云之间存在辐射相互作用的单层破碎云场的情况。在这种情况下,重正化系数也取决于云之间的距离。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Correction of cloud optical thickness retrievals from nadir reflectances in the presence of 3D radiative effects. Part I: concept and tests on 3D RT simulations
3D effects cause substantial underestimation of cloud optical thickness (COT) in airborne and satellite retrievals based on 1D radiative transfer computations (such as in the case of widely used bispectral technique). For a single-layer isolated cloud we propose a simple linear correction of the retrieved COT with the renormalization factor dependent on the cloud’s aspect ratio (the ratio between vertical and horizontal dimensions of the cloud). This is an empirical assumption which we successfully test using synthetic 3D RT data. We introduce a heuristic “block model” of 3D radiative effects and show that the functional form of the renormalization factor is consistent with the process of radiation escape from cloud sides in an essentially 3D geometry. We also extend the block model to the case of single-layer broken cloud field with radiative interaction between the neighboring clouds. In this case the renormalization factor depends also on the distance between clouds.
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