To Evaluate the Characteristics of Cloud Parameters Retrieved by Satellite and Cloud Structure of the Northward Typhoon In-Fa

Xiaorui Zhang, W. Yang, T. Hou, Zhiqiang Shen, Shuai Li, Shaoyu Hou, Jing Meng
{"title":"To Evaluate the Characteristics of Cloud Parameters Retrieved by Satellite and Cloud Structure of the Northward Typhoon In-Fa","authors":"Xiaorui Zhang, W. Yang, T. Hou, Zhiqiang Shen, Shuai Li, Shaoyu Hou, Jing Meng","doi":"10.5220/0011024600003354","DOIUrl":null,"url":null,"abstract":"Cloud parameters retrieved by Satellite and model data with detailed cloud microphysical processes are used in this paper to conduct a comprehensive analysis of the precipitation process of the northward typhoon \"Infa\" in Hebei Province. The main conclusions are as follows: optical thickness (>20), cloud top temperature (10°C~-25°C), and cloud top height (>9km) of cloud characteristics parameters retrieved by FY-2 satellite (Fengyun meteorological satellite) have obvious indications for the range and intensity of precipitation. The effective radius of cloud particles needs to be combined with multi-parameter comprehensive analysis. Satellite monitoring products can be used to compare and correct cloud model forecast products. In the early stage of the low-pressure precipitation process of this typhoon, cold clouds are thicker, and the content of hydrometeor and supercooled water in cold clouds are abundant. After 17:00 on the 29th, the hydrometeor and supercooled water contents of cold clouds have decreased significantly and increased obviously in warm cloud, the large value center of water content have also decreased, ice crystals number concentration and snow-graupel mixing ratio have declined, and the main precipitation mechanism changed from cold cloud precipitation to warm cloud precipitation.","PeriodicalId":249714,"journal":{"name":"Proceedings of The International Conference on Water Resource and Environment","volume":"63 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Proceedings of The International Conference on Water Resource and Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5220/0011024600003354","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

Cloud parameters retrieved by Satellite and model data with detailed cloud microphysical processes are used in this paper to conduct a comprehensive analysis of the precipitation process of the northward typhoon "Infa" in Hebei Province. The main conclusions are as follows: optical thickness (>20), cloud top temperature (10°C~-25°C), and cloud top height (>9km) of cloud characteristics parameters retrieved by FY-2 satellite (Fengyun meteorological satellite) have obvious indications for the range and intensity of precipitation. The effective radius of cloud particles needs to be combined with multi-parameter comprehensive analysis. Satellite monitoring products can be used to compare and correct cloud model forecast products. In the early stage of the low-pressure precipitation process of this typhoon, cold clouds are thicker, and the content of hydrometeor and supercooled water in cold clouds are abundant. After 17:00 on the 29th, the hydrometeor and supercooled water contents of cold clouds have decreased significantly and increased obviously in warm cloud, the large value center of water content have also decreased, ice crystals number concentration and snow-graupel mixing ratio have declined, and the main precipitation mechanism changed from cold cloud precipitation to warm cloud precipitation.
北上台风“银发”卫星云参数反演特征及云结构分析
本文利用卫星反演的云参数和具有详细云微物理过程的模式资料,对北上台风“Infa”在河北地区的降水过程进行了综合分析。主要结论是:风云气象卫星(FY-2)反演的云特征参数光学厚度(>20)、云顶温度(10°C~-25°C)和云顶高度(>9km)对降水的范围和强度有明显的指示作用。云粒子的有效半径需要结合多参数综合分析。卫星监测产品可以用来比较和校正云模式预报产品。本次台风低压降水过程前期,冷云较厚,冷云中水流星和过冷水含量丰富。29日17时以后,冷云中水流星和过冷水含量明显减少,暖云中水流星和过冷水含量明显增加,含水量大值中心也减少,冰晶数浓度和雪霰混合比下降,主要降水机制由冷云降水转变为暖云降水。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信