使用地基剖面辐射计观测渥太华上空含液层积云的衰减

P. Bouchard
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引用次数: 4

摘要

本文介绍了渥太华上空非降水、含液体的阴天层积云(Sc)在白天造成的衰减统计。从地面多频剖面辐射计的亮度温度数据和反演数据中提取了Sc云衰减的时间序列。感兴趣的频率是30 GHz和51.25 GHz;考虑15到90度(天顶)之间的四个仰角。MPM psila93和Rosenkranz模型都被用来评估气体吸收,利用从当地站点获取的最接近时间的无线电探空仪数据来获取剖面。由于数据集中的大多数云都包含一些过冷液体,因此将这些提取的云衰减数据与使用同时检索的液态水路径数据和云基温度作为输入的各种纯液态水介电常数模型的预测结果进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observations of attenuation due to liquid-bearing stratocumulus clouds over Ottawa using a ground-based profiling radiometer
Statistics on the attenuation due to non-precipitating, liquid-bearing overcast stratocumulus (Sc) clouds over Ottawa during the daytime are presented in this paper. Time series of Sc cloud attenuation are extracted from the brightness temperature data and retrievals from a ground-based multifrequency profiling radiometer. Frequencies of interest are 30 and 51.25 GHz; four elevation angles between 15 and 90 degrees (zenith) are considered. Both the MPM psila93 and Rosenkranz models are used to assess gaseous absorption using retrieved profiles ldquotopped uprdquo with the closest in time radiosonde data from a local station. Since most of the clouds in the data set contain some supercooled liquid, these extracted cloud attenuation data are compared to predictions from various dielectric constant models for pure liquid water using both the contemporaneously-retrieved liquid water path data and temperature at the cloud base as inputs.
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