台风“苏拉”登陆福建后降水的非对称成因分析
作者:
基金项目:

中国气象局预报员专项项目(CMAYBY2014-034);中国气象局关键技术集成项目(GMAGJ2015M30)


Analysis of the precipitation asymmetries of typhoon Saola after its landfall on Fujian Province
Author:
  • 摘要
  • | |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
  • |
    摘要:

    利用常规天气资料、NCEP再分析资料、卫星云图、新一代天气雷达等资料,分析了2012年第9号台风"苏拉"降水预报失败的原因及其暴雨成因。结果表明:此次台风暴雨预报失败的主要原因在于预报过程中没有关注台风垂直结构的改变及其对降水落区的影响。"苏拉"台风暴雨是在中高纬稳定的环流形势下发生的,低层到高层引导气流的变化导致"苏拉"高层风暴中心向南倾斜;环境风垂直切变导致了台风降水的非对称分布,环境风垂直切变方向的左侧是强降水发展的区域;此外,随着台风环流中心在垂直方向发生偏移,改变了涡度平流的垂直分布,从而导致了福建省南部的暴雨。因此关注登陆台风中心在垂直方向的偏移对台风降水预报非常重要。

    Abstract:

    By using the conventional meteorological data,NCEP 1°×1° reanalysis data,Satellite Images data and CINRAD/SA data,the reason for the failure of the foecast and the cause of the heavy rainfall after Saola Typhoon landing is analyzed.Asymmetric distribution of precipitation by Typhoon Saola has been analyzed from circulation background,change of vertical structure,steering flows,environmental vertical windshear,physical quantity diagnosis and so on.The results show that:The main reason for the large deviation of typhoon rainstorm forecast and actual situation is that little attention has been paid to the change of the vertical structure of typhoon and its impact on the precipitation area during the forecasting process.The stable circulation background of high latitude provides favorable conditions of asymmetric distribution of typhoon precipitation;the change of steering flows in the vertical tilted the typhoon center southward with height;the steering flows and environmental vertical wind shear are the reasons which caused the typhoon center southward with height;The change of the vertical wind shear indicates the heavy rainfall region,which reflects the stronger convection and rain on the left of downshear;In addition,while the typhoon center southward with height,the distribution of the vorticity has to been changed,so the heavy rainfall happened in the southern Fujian proivince.Therefore,it is important to pay attention to the change of this vertical structure of typhoon.

    参考文献
    Chen L S,Luo Z X,1995.Some relations between asymmetric structure and motion of typhoon[J].Acta Meteor Sinica,9(4):412-419.
    Chen S S,Knaff J A,Marks Jr F D,2006.Effects of vertical wind shear and storm motion on tropical cyclone rainfall asymmetries deduced from TRMM[J].Mon Wea Rev,134:3190-3208.
    丁金才,姚祖庆,唐新章,1997.9414号热带气旋(DOUG)非对称结构和对降水的影响分析[J].气象学报,55(3):379-384. Ding J C,Yao Z Q,Tang X Z,1997.The analysis of the asymmetric structure of tropical cyclone Doug and its influence on precipitation[J].Acta Meteorologica Sinica,55(3):379-384.(in Chinese).
    Frank W M,Ritchie E A,2001.Effects of vertical wind shear on the intensity and structure of numerically simulated hurricanes[J].Mon Wea Rev,129:2249-2269.
    李杭玥,王咏青,辛辰,2015.飓风Bonnie发生发展过程中的强度结构变化和惯性稳定度分析[J].大气科学学报,38(1):27-36. Li H Y,Wang Y Q,Xin C,2015.An analysis of intensity and structural changes in relation to intertial stability during the development of Hurricane Bonnie(1998)[J].Trans Atmos Sci,38(1):27-36.(in Chinese).
    李英,陈联寿,徐祥德,2005.水汽输送影响登陆热带气旋维持和降水的数值试验[J].大气科学,29(1):91-98. Li Y,Chen L S,Xu X D,2005.Numerical experiment of the impact of moisture transportation on sustaining of the landfalling tropical cyclone and precipition[J].Chin J Atmos Sci,29(1):91-98.(in Chinese).
    李勋,李泽椿,赵声蓉,等,2010."珍珠"(0601)异常急翘路径和内核结构变化的诊断分析及数值研究[J].气象,36(9):1-8. Li X,Li Z C,Zhao S R,et al.,2010.A diagnosis and numerical study of an abrupt recurved typhoon Chanchu and its inner core structure evolution[J].Meteor Mon,36(9):1-8.(in Chinese).
    毛丽娜,潘益农,2009.环境风垂直切变对热带气旋"碧利斯"的影响[J].气象科学,29(4):507-512. Mao L N,Pan Y N,2009.Influence of environmental vertical wind shear on tropical cyclone Bilis[J].Scientia Meteorologica Sinica,29(4):507-512.(in Chinese).
    钮学新,杜惠良,刘建勇,2005.0216号台风降水及其影响降水机制的数值模拟试验[J].气象学报,63(1):57-68. Niu X X,Du H L,Liu J Y,2005.The numerical simulation of rainfall and precipitation mechanism associated with typhoon SinlaKu(0216)[J].Acta Meteorologica Sinica,63(1):57-68.(in Chinese).
    Palmer C,Barnes G,2002.The effect of vertical wind shear as diagnosed by the NCEP/NCAR reanalysis data on northeast Pacific hurricane intensity[C]//AMS.25th conf on hurricanes and tropical meteorology,sandiego:CA:122-123.
    舒守娟,王远,宋金杰,2011.西北太平洋台风"海棠"结构的GPS下投式探空仪观测分析[J].气象学报,69(6):933-944. Shu S J,Wang Y,Song J J,2011.Observational analysis of the structure of typhoon Haitang(0505) over the western North Pacific by using the GPS porpsonde data[J].Acta Meteorologica Sinica,69(6):933-944.(in Chinese).
    陶祖钰,田佰军,黄伟,1994.9216号台风登陆后的不对称结构和暴雨[J].热带气象学报,10(1):69-77. Tao Z Y,Tian B J,Huang W,1994.Asymmetry structure and torrential rain of landing typhoon 9216[J].J Trop Meteor,10(1):69-77.(in Chinese).
    王长甫,余荣华,刘福晓,1991.多层加权平均引导台风路径预报方法[J].应用气象学报,2(4):434-439. Wang C F,Yu R H,Liu F X,1991.A multiple-layer weighted mean steering method of the typhoon track forecast[J].Quarterly Journal of Applied Meteorologica Science,2(4):434-439.(in Chinese).
    王伟,余锦华,2013.东风和西风切变环境下西北太平洋热带气旋快速增强特征的对比[J].大气科学学报,36(3):337-345. Wang W,Yu J H,2013.Characteristic comparison between the rapid intensification of tropical cyclones in easterly and westerly wind shear over the Northwest Pacific[J].Trans Atmos Sci,36(3):337-345.(in Chinese).
    魏超时,赵坤,余晖,等,2011.登陆台风卡努(0515)内核区环流结构特征分析[J].大气科学,35(1):68-80. Wei C S,Zhao K,Yu H,et al.,2011.Mesoscale structure of landfall typhoon Khanun(0515) by single Doppler radar[J].Chin J Atmos Sci,35(1):68-80.(in Chinese).
    Wu L G,Braun S A,Halverson J,et al.,2006.A numerical study of hurricane Erin(2001).Part I:Model verification and storm evolution[J].J Atmos Sci,62:65-86.
    吴乃庚,林良旭,李天然,等,2007.环境流场和"派比安"结构变化对其异常北抬路径影响的诊断分析[J].气象,33(11):9-15. Wu N G,Lin L X,Li T R,et al.,2007.Diagnosis of northward-deflecting track of typhoon Prapiroon caused by the environmental flow field and typhoon structure variation[J].Meteor Mon,33(11):9-15.(in Chinese).
    余贞寿,高守亭,任鸿翔,2007a.台风"海棠"特大暴雨数值模拟研究[J].气象学报,65(6):864-876. Yu Z S,Gao S T,Ren H X,2007a.A numerical study of the severe heavy rainfall associated with the typhoon Haitang[J].Acta Meteorologica Sinica,65(6):864-876.(in Chinese).
    余贞寿,郝增周,谢海华,等,2007b.台湾岛地形对台风"海棠"(0505)移动路径影响的数值试验研究[J].热带气象学报,23(6):575-580. Yu Z X,Hao Z Z,Xie H H,et al.,2007b.A numerical study of the effect of Taiwan island terrain on typhoon Haitang(0505) track[J].J Trop Meteor,23(6):575-580.(in Chinese).
    Zhang D L,Chanh Q,Kieu,2005.Shear-forced vertical circulations in tropical cyclones[J].Geophys Res Letters,32(13):301-320.
    赵海坤,吴立广,2015.西北太平洋热带气旋气候变化的若干研究进展[J].气象科学,35(1):108-118. Zhao H K,Wu L G,2015.Review on climate change of tropical cyclone in the Northwest Pacific[J].J Meteor Sci,35(1):108-118.(in Chinese).
    赵海坤,赵伟荣,赵军平,2013.西北太平洋热带气旋频数年际变化的统计预测[J].统计与决策,(21):81-85. Zhao H K,Zhao W R,Zhao J P,2013.Satistical prediction of inter-annual variation of the western North Pacific tropical cyclone frequecy[J].Statistics and Decision,(21):81-85.(in Chinese).
    朱乾根,林锦瑞,寿绍文,等,2000.天气学原理与方法[M].4版.北京:气象出版社. Zhu Q G,Lin J R,Shou S W,et al.,2000.Weather princilples and methods[M].4th ed. Beijing:Beijing Meteorological Press.(in Chinese).
    网友评论
    网友评论
    分享到微博
    发 布
引用本文

蔡菁,吴立广,赖巧珍,冯晋勤,危国飞,2017.台风“苏拉”登陆福建后降水的非对称成因分析[J].大气科学学报,40(6):814-822. CAI Jing, WU Liguang, LAI Qiaozhen, FENG Jinqin, WEI Guofei,2017. Analysis of the precipitation asymmetries of typhoon Saola after its landfall on Fujian Province[J]. Trans Atmos Sci,40(6):814-822. DOI:10.13878/j. cnki. dqkxxb.20170222001

复制
分享
文章指标
  • 点击次数:1417
  • 下载次数: 2385
  • HTML阅读次数: 0
  • 引用次数: 0
历史
  • 收稿日期:2017-02-22
  • 最后修改日期:2017-06-28
  • 在线发布日期: 2017-12-27

地址:江苏南京宁六路219号南京信息工程大学    邮编:210044

联系电话:025-58731158    E-mail:xbbjb@nuist.edu.cn    QQ交流群号:344646895

大气科学学报 ® 2025 版权所有  技术支持:北京勤云科技发展有限公司