NUMERICAL STUDY OF COLD AIR IMPACT ON RAINFALL REINFORCEMENT ASSOCIATED WITH TROPICAL CYCLONE TALIM(2005):I.IMPACT OF DIFFERENT COLD AIR INTENSITY

In 2005,significant rainfall reinforcement and severe disaster was induced by tropical cyclone(TC) Talim after it made landfall on the east of China.Observational analyses show that it has relationship with cold air intrusion.For investigating the impact of cold air intensity,we make use of Weather...

Full description

Saved in:
Bibliographic Details
Published in热带气象学报:英文版 no. 1; pp. 87 - 96
Main Author 董美莹 陈联寿 李英 程正泉 郑沛群
Format Journal Article
LanguageEnglish
Published 2013
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:In 2005,significant rainfall reinforcement and severe disaster was induced by tropical cyclone(TC) Talim after it made landfall on the east of China.Observational analyses show that it has relationship with cold air intrusion.For investigating the impact of cold air intensity,we make use of Weather Research and Forecasting(WRF) model,the synthesizer of NCEP/NCAR reanalysis data and Japan regional spectral model data,to carry out numerical experiments.Results show that rainfall reinforcement occurs in all experiments.Different intensity of cold air can modify the rainfall distribution and intensity significantly.In the rainfall center,the increment maximum of rainfall is twice as large as that of the minimum.Moderate cold air intrusion may result in the strongest rainfall reinforcement.Different cold air intensity can lead to different motion of low-level convergence lines and fronts.There is a good relationship between the rainfall region and the eastern part of the front.On one hand,strong cold air weakens the TC intensity by its intrusion into the TC center and results in weak convergence and a convergent zone and a rain band shifted southward.On the other hand,weak cold air reduces the convergence and moves the convergent zone and rain band northward.Moderate cold air intrusion maintains strong low-level convergence and high-level divergence,keeping strong upward motion over certain regions.Consequently,the rain band begins to stagnate and rainfall reinforces abruptly therein.
Bibliography:44-1409/P
DONG Mei-ying1,CHEN Lian-shou 2,LI Ying 2,CHENG Zheng-quan 3,ZHENG Pei-qun 4(1.Zhejiang Institute of Meteorological Sciences,Hangzhou 310008 China;2.State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081 China;3.Guangdong Provincial Meteorological Observatory,Guangzhou 510080 China;4.Zhejiang Provincial Meteorological Observatory,Hangzhou 310017 China)
ISSN:1006-8775