首页期刊介绍通知公告编 委 会投稿须知电子期刊广告合作联系我们在线留言
 
台风“摩羯”(2018年)登陆台州并造成台州大暴雨的成因分析
作者:倪钟萍1  魏雪1  贺立夫2  裘杭培1 
单位:1. 台州市气象局, 浙江 台州 318000;
2. 台州市路桥区气象局, 浙江 台州 318050
关键词:登陆台风 大暴雨 涡度趋势 雷达 
分类号:P444
出版年·卷·期(页码):2022·39·第四期(37-46)
摘要:
利用自动站气象要素资料、FNL全球分析资料和台州雷达资料,分析台风“摩羯”(2018年)登陆台州并造成台州大暴雨的原因。结果表明:涡度趋势分析发现,登陆前正相对涡度趋势大值区位于台州南部—温州北部地区,指示台风“摩羯”向其沿海靠近,最后登陆于台州南部的温岭沿海,其主要贡献是涡度平流项即副热带高压对台风的引导作用。台风“摩羯”给台州带来的大暴雨主要位于黄岩、仙居、临海和天台交界的山区,为台风本体带来的降水,东—东南风急流配合深厚的水汽条件以及台风的不对称结构和台州西部山区的地形增幅作用造成了局地大暴雨。此次过程中,雨量最大的天柱林场地区81%时次的降水是在回波强度达25 dBZ以上时产生的,回波最强达47 dBZ时6 min雨量为6.1 mm,25~40 dBZ的回波强度平均产生1.25 mm/6 min的降水;“摩羯”台风降水的回波强度不强,但较强降水持续近11 h,累计雨量达大暴雨。
The reason for typhoon "Yagi" (2018) making landfall and causing heavy rainfall in Taizhou is analyzed using the meteorological data of medium-scale automatic meteorological stations, global Final Analysis (FNL) analysis data and radar data in Taizhou. The results show that the positive relative vorticity tendency with large value before the landfall is located between the south of Taizhou and the north of Wenzhou, indicating that the typhoon approaches the coast of Wenzhou and Taizhou. The landing of typhoon "Yagi" in the coast of Wenling in southern Taizhou in the end is mainly due to the vorticity advection, which is the guiding effect of the subtropical high on typhoon "Yagi". The heavy rainfall caused by typhoon "Yagi" is mainly located in mountainous areas at the junction of Huangyan, Xianju, Linhai and Tiantai, which is caused by the typhoon itself. The local heavy rainfall is caused by the east-southeast wind jet bring deep water vapor, the asymmetry structure of typhoon and the topographic amplification effect of the western mountainous area of Taizhou. During this process, the heaviest rainfall locates in the Tianzhu Forest Farm area, and 81% of the precipitation is generated when the echo intensity is above 25 dBZ. When the echo is the strongest at 47 dBZ, the rainfall in 6 min is 6.1 mm, and the echo intensity of 25~40 dBZ produces 1.25 mm of precipitation per 6 min on average. The echo intensity of typhoon "Yagi" precipitation is not strong. However, the heavy rainfall lasts for nearly 11 hours and causes the heavy rain.
参考文献:
[1] 刘庭杰,施能,顾骏强.浙江省台风灾害的统计分析[J].灾害学, 2002, 17(4):64-71. LIU T J, SHI N, GU J Q. A statistical analysis of typhoon disasters in Zhejiang province[J]. Journal of Catastrophology, 2002, 17(4):64-71.
[2] 张娇艳,吴立广,张强.全球变暖背景下我国热带气旋灾害趋势分析[J].热带气象学报, 2011, 27(4):442-454. ZHANG J Y, WU L G, ZHANG Q. Tropical cyclone damages in China under the background of global warming[J]. Journal of Tropical Meteorology, 2011, 27(4):442-454.
[3] 王镇铭,杜惠良,杨诗芳.浙江省天气预报手册[M].北京:气象出版社, 2013. WANG Z M, DU H L, YANG S F. Weather forecast manual in Zhejiang province[M]. Beijing:China Meteorological Press, 2013.
[4] 端义宏,陈联寿,梁建茵,等.台风登陆前后异常变化的研究进展[J].气象学报, 2014, 72(5):969-986. DUAN Y H, CHEN L S, LIANG J Y, et al. Research progress in the unusual variations of typhoons before and after landfalling[J]. Acta Meteorologica Sinica, 2014, 72(5):969-986.
[5] 范爱芬,彭霞云,娄小芬,等.台风"鮎鱼"极端降水分析[J].气象科技, 2019, 47(1):79-88. FAN A F, PENG X Y, LOU X F, et al. Extreme precipitation analysis of typhoon Megi[J]. Meteorological Science and Technology, 2019, 47(1):79-88.
[6] 吴海英,陈海山,曾明剑,等.冷空气对台风"海葵"(1211)倒槽特大暴雨作用分析[J].热带气象学报, 2014, 30(5):871-880. WU H Y, CHEN H S, ZENG M J, et al. Analysis on the functions of cold air in a super heavy rainfall caused by a reverse trough of typhoon Haikui (1211)[J]. Journal of Tropical Meteorology, 2014, 30(5):871-880.
[7] 刘建勇,周冠博,顾思南,等.台风菲特暴雨诊断分析[J].气象科技, 2014, 42(6):1047-1056. LIU J Y, ZHOU G B, GU S N, et al. Diagnosis of heavy rainfall associated with typhoon Fitow[J]. Meteorological Science and Technology, 2014, 42(6):1047-1056.
[8] 张树民,王坤,孙刚,等.台风尼伯特(1601)残留低压局地大暴雨成因分析[J].气象科技, 2018, 46(1):139-148. ZHANG S M, WANG K, SUN G, et al. Effect of residual low of typhoon Nepartak on a local extraordinary rainstorm[J]. Meteorological Science and Technology, 2018, 46(1):139-148.
[9] 杨舒楠,陈涛,刘建勇.两次台风暴雨冷空气影响对比分析[J].气象科技, 2018, 46(2):324-335. YANG S N, CHEN T, LIU J Y, et al. Comparative analysis of TC rainstorms induced by cold air intrusion of two TC cases[J]. Meteorological Science and Technology, 2018, 46(2):324-335.
[10] 李英,陈联寿,徐祥德.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, 2005, 29(1):91-98. LI Y, CHEN L S, XU X D. Numerical experiments of the impact of moisture transportation on sustaining of the landfalling tropical cyclone and precipitation[J]. Chinese Journal of Atmospheric Sciences, 2005, 29(1):91-98.
[11] 黄克慧,陈宣淼,楼茂园,等.台风倒槽浙江暴雨的"配料法"研究[J].科技通报, 2019, 35(9):12-21. HUANG K H, CHEN X M, LOU M Y, et al. Study of ingredientsbased methodology of Zhejiang torrential rainfall in typhoon inverted trough[J]. Bulletin of Science and Technology, 2019, 35(9):12-21.
[12] 方艳莹,钱燕珍,申华羽,等. 1822号台风"山竹"引起浙江东北部大暴雨成因分析[J].海洋预报, 2020, 37(4):86-96. FANG Y Y, QIAN Y Z, SHEN H Y, et al. Causes analysis on the heavy rainfall in northeastern Zhejiang related to the typhoon "Mangkhut" (1822)[J]. Marine Forecasts, 2020, 37(4):86-96.
[13] 王毅,钱燕珍,段晶晶,等."温比亚"台风登陆前后大暴雨特征及成因分析[J].海洋预报, 2020, 37(3):62-71. WANG Y, QIAN Y Z, DUAN J J, et al. Analysis on the characteristics and reasons of the heavy rainfall caused by landfalling typhoon "Rumbia" [J]. Marine Forecasts, 2020, 37(3):62-71.
[14] 陈联寿,丁一汇.西太平洋台风概论[M].北京:科学出版社, 1979. CHEN L S, DING Y H. Introduction to Western Pacific typhoon[M]. Beijing:Science Press, 1979.
[15] 陈联寿,孟智勇.我国热带气旋研究十年进展[J].大气科学, 2001, 25(3):420-432. CHEN L S, MENG Z Y. An overview on tropical cyclone research progress in China during the past ten years[J]. Chinese Journal of Atmospheric Sciences, 2001, 25(3):420-432.
[16] 陈宏义,袁鸿生.温台地区长驱直袭型热带气旋登陆前后降水分布特征初探[C]//第28届中国气象学会年会--S12热带气旋.厦门:中国气象学会, 2011. CHEN H Y, YUAN H S. A preliminary analysis on the distribution of precipitation before and after the tropical cyclone direct landfall in Wenzhou and Taizhou[C]//The 28th Annual Meeting of the Chinese Meteorological Society-S12 Tropical Cyclone.
[17] 裘杭培,李恭彪.台风"莫拉克"引发降水成因初步分析[C]//第27届中国气象学会年会灾害天气研究与预报分会场论文集.北京:中国气象学会, 2010:2608-2613. QIU H P, LI G B. A preliminary analysis on the causes of precipitation caused by typhoon "Morakot" [C]//The Proceedings of the 27th Annual Meeting of the Chinese Meteorological Society on Disaster Weather Research and Forecast. Beijing:Chinese Meteorological Society, 2010:2608-2613.
[18] CHAN J C L. An observational study of the physical processes responsible for tropical cyclone motion[J]. Journal of the Atmospheric Sciences, 1984, 41(6):1036-1048.
[19] WU L G, NI Z P, DUAN J J, et al. Sudden tropical cyclone track changes over the Western North Pacific:a composite study[J]. Monthly Weather Review, 2013, 141(8):2597-2610.
[20] 段晶晶,吴立广,倪钟萍. 2004年台风"艾利"与"米雷"路径异常变化分析[J].气象学报, 2014, 72(1):1-11. DUAN J J, WU L G, NI Z P. Analysis of unusual changes in typhoon Aere (2004) and Meari (2004)[J]. Acta Meteorologica Sinica, 2014, 72(1):1-11.
[21] 许映龙,刘震坤,董林,等. 2002年西北太平洋和南海热带气旋路径主客观预报评价[J].气象, 2005, 31(6):43-46. XU Y L, LIU Z K, DONG L, et al. Verification of subjective and objective track forecast of Tropical cyclones over Northwest Pacific and South China Sea in 2002[J]. Meteorological Monthly, 2005, 31(6):43-46.
[22] 倪钟萍,吴立广,张玲. 2005-2010年台风突变路径的预报误差及其环流背景[J].气象, 2013, 39(6):719-727. NI Z P, WU L G, ZHANG L. Analysis on Forecasting errors and associated circulations of sudden typhoon track changes during 2005-2010[J]. Meteorological Monthly, 2013, 39(6):719-727.
[23] 陈联寿.热带气旋研究和业务预报技术的发展[J].应用气象学报, 2006, 17(6):672-681. CHEN L S. The evolution on research and operational forecasting techniques of tropical cyclones[J]. Journal of Applied Meteorological Science, 2006, 17(6):672-681.
服务与反馈:
文章下载】【发表评论】【查看评论】【加入收藏
 
 海洋预报编辑部 地址:北京海淀大慧寺路8号
电话:010-62105776
投稿网址:http://www.hyyb.org.cn
邮箱:bjb@nmefc.cn