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对强台风“纳沙”(1117)登陆海南岛前后降水非对称性的分析

周海波 白爱娟 蔡亲波

热带气象学报2017,Vol.33Issue(3):386-398,13.
热带气象学报2017,Vol.33Issue(3):386-398,13.DOI:10.16032/j.issn.1004-4965.2017.03.010

对强台风“纳沙”(1117)登陆海南岛前后降水非对称性的分析

ANALYSIS ON ASYMMERIC PRECIPITATION OFTHE STRONG TYPHOON NESAT (1117) BEFOREAND AFTER LANDING ON HAINAN ISLAND

周海波 1白爱娟 1蔡亲波2

作者信息

  • 1. 成都信息工程大学大气科学学院,四川成都610225
  • 2. 海南省气象台,海南海口570203
  • 折叠

摘要

Abstract

Using the NCEP 1 °×1 o reanalysis data,satellite data,this paper takes the strong typhoon Nesat in 2011 for example to analyze the precipitation characteristics of the typhoon before and after landing on Hainan Island,and the asymmetry characteristics of TBB,humidity,horizontal wind speed and vertical velocity surrounding the typhoon on the left and right sides of the path,and discuss the possible causes of precipitation distribution from the aspect of the distribution of spatial structure.The results are showed as follows.Before and after landing on Hainan Island,the precipitation distribution of typhoon Nesat showed significant asymmetry,and heavy rainfall mainly concentrated on the left side of the path.In addition to relatively symmetricaltemperature anomalies,other physical quantities surrounding the typhoon showed significant asymmetry in the following points:(1) TBB.The intensity of strong convective clouds was greater,its range on the left side was larger than on the right side;(2) Moisture.The range of wet area on the left side was larger than on the right side;(3) Horizontal wind field.The maximum wind speed on the right side were stronger than on the left side when the typhoon was at sea and landed,especially when the typhoon landed maximum wind speed difference between the sides was up to 20rn/s;the range of equal maximum wind speed on the right side was wider than on the left side before and after the landing of the typhoon;(4) Vertical velocity.Upward motion on the left side was stronger than on the right side,especially vertical rising velocity on the left side was-2.4 Pa/s stronger than on the right side when the typhoon landed.By comparing the distribution of the above physicswith the distribution of precipitation,we found that humidity may be one reason for the asymmetric distribution of precipitation,and the vertical speed may be the main reason for asymmetric precipitation of typhoon Nesat.From the vertical wind shear,we further explored the role of the formation mechanism of asymmetric typhoon precipitation and found that the heavy rainfall was concentrated in the shear direction and along the left side before and after the typhoon landed on Hainan Island.Vertical wind shear can better explain the strong vertical upward movement and heavy precipitation area on the left side of the path.In addition,Hainan Island terrain conditions also led to a significant increase in typhoon precipitation in the western part of theisland during the landing of typhoon Nesat.

关键词

海南岛/强台风“纳沙”/非对称降水/空间结构/垂直风切变

Key words

Hainan Island/strong typhoon Nesat/distribution of asymmetric precipitation/spatial structure/vertical wind shear

分类

天文与地球科学

引用本文复制引用

周海波,白爱娟,蔡亲波..对强台风“纳沙”(1117)登陆海南岛前后降水非对称性的分析[J].热带气象学报,2017,33(3):386-398,13.

基金项目

国科技部国家科技支撑计划项目(2013BAK05B03)资助 (2013BAK05B03)

热带气象学报

OA北大核心CSCDCSTPCD

1004-4965

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