Bulk Scattering Properties for the Remote Sensing of Ice Clouds. Part I: Microphysical Data and Models.

B. Baum, A. Heymsfield, P. Yang, S. Bedka
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引用次数: 274

Abstract

This study reports on the use of in situ data obtained in midlatitude and tropical ice clouds from airborne sampling probes and balloon-borne replicators as the basis for the development of bulk scattering models for use in satellite remote sensing applications. Airborne sampling instrumentation includes the twodimensional cloud (2D-C), two-dimensional precipitation (2D-P), high-volume precipitation spectrometer (HVPS), cloud particle imager (CPI), and NCAR video ice particle sampler (VIPS) probes. Herein the development of a comprehensive set of microphysical models based on in situ measurements of particle size distributions (PSDs) is discussed. Two parameters are developed and examined: ice water content (IWC) and median mass diameter Dm. Comparisons are provided between the IWC and Dm values derived from in situ measurements obtained during a series of field campaigns held in the midlatitude and tropical regions and those calculated from a set of modeled ice particles used for light-scattering calculations. The ice particle types considered in this study include droxtals, hexagonal plates, solid columns, hollow columns, aggregates, and 3D bullet rosettes. It is shown that no single habit accurately replicates the derived IWC and Dm values, but a mixture of habits can significantly improve the comparison of these bulk microphysical properties. In addition, the relationship between Dm and the effective particle size Deff, defined as 1.5 times the ratio of ice particle volume to projected area for a given PSD, is investigated. Based on these results, a subset of microphysical models is chosen as the basis for the development of ice cloud bulk scattering models in Part II of this study.
冰云遥感体散射特性研究。第一部分:微物理数据和模型。
本研究报告利用空中采样探测器和气球复制器在中纬度和热带冰云中获得的现场数据,作为发展用于卫星遥感应用的体散射模型的基础。机载采样仪器包括二维云(2D-C)、二维降水(2D-P)、大体积降水光谱仪(HVPS)、云粒子成像仪(CPI)和NCAR视频冰粒子采样器(VIPS)探测器。本文讨论了一套基于原位测量粒度分布(psd)的综合微物理模型的发展。提出并检查了两个参数:冰水含量(IWC)和中位质量直径Dm。在中纬度和热带地区进行的一系列野外活动中获得的IWC和Dm值与用于光散射计算的一组模拟冰粒计算得到的Dm值进行了比较。本研究考虑的冰颗粒类型包括:柱状、六边形板状、实心柱状、空心柱状、聚集体状和三维弹状玫瑰花状。结果表明,没有一种习惯能准确地复制所得的IWC和Dm值,但混合习惯可以显著改善这些散装微物理特性的比较。此外,研究了Dm与有效粒径Deff之间的关系,Deff定义为给定PSD下冰颗粒体积与投影面积之比的1.5倍。基于这些结果,本研究的第二部分选择了一个微物理模型子集作为开发冰云体散射模型的基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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