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利用热带降雨测量卫星任务获取的中美地区雹暴特性

Properties of hail storms over China and the United States from the Tropical Rainfall Measuring Mission.

作者信息

Ni Xiang, Liu Chuntao, Zhang Qinghong, Cecil Daniel J

机构信息

Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, China.

Department of Physical and Environmental Sciences, Texas A&M University at Corpus Christi, Texas, USA.

出版信息

J Geophys Res Atmos. 2016 Oct 27;121(20):12031-12044. doi: 10.1002/2016JD025600. Epub 2016 Oct 25.

Abstract

A 16-yr record of hail reports over the south U.S. and from weather stations in China are collocated with Precipitation Features (PF) derived from the Tropical Rainfall Measuring Mission (TRMM) radar and passive microwave observations. Differences in the way hail is reported in the two nations make it difficult to draw meaningful conclusions about storm frequency. But taking the two together yields a wide spectrum of hail sizes, suitable for comparing with remote sensing measurements. While U.S. hail reports are dominated by cases with hail size greater than 19 mm, hail reports in China mostly include diameters of 1-10 mm and mostly occur over the Tibetan Plateau. The fraction of PFs collocated with hail reports (hail PFs) reaches 3% in the plains of the U.S. In China, the fraction is higher in high elevation regions than low elevation regions. Hail PFs (as reported in the U.S.) show lower brightness temperatures, higher lightning flash rates, stronger maximum reflectivity, and higher echo tops than those with smaller hail, as reported in China. The average near surface maximum reflectivity of hail PFs at high elevations (≥ 2000 m) in China is about 5 dB smaller than those at low elevations. Larger hail is reported with PFs having stronger maximum reflectivity above 6 km, though the median of maximum reflectivity values at levels below 5 km is similar among the storms with large and small hail sizes.

摘要

美国南部的16年冰雹报告记录以及来自中国气象站的数据,与源自热带降雨测量卫星(TRMM)雷达和被动微波观测的降水特征(PF)进行了搭配。两国在冰雹报告方式上的差异使得难以就风暴频率得出有意义的结论。但将两者结合起来会产生各种各样的冰雹尺寸,适合与遥感测量结果进行比较。虽然美国的冰雹报告主要是冰雹尺寸大于19毫米的情况,但中国的冰雹报告大多包括直径为1 - 10毫米的冰雹,且大多发生在青藏高原。在美国平原地区,与冰雹报告搭配的PF比例(冰雹PF)达到3%。在中国,高海拔地区的这一比例高于低海拔地区。与中国报告的较小冰雹相比,美国报告的冰雹PF显示出更低的亮温、更高的闪电闪率、更强的最大反射率和更高的回波顶。中国高海拔(≥2000米)地区冰雹PF的近地表平均最大反射率比低海拔地区小约5分贝。尽管大小冰雹风暴在5千米以下高度的最大反射率值中位数相似,但报告较大冰雹时对应的PF在6千米以上具有更强的最大反射率。

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