nav emailalert searchbtn searchbox tablepage yinyongbenwen piczone journalimg qikanlogo popupnotification paper
2025 03 v.55 1-12
2019年超强台风“利奇马”外雨带降水精细结构分析
基金项目(Foundation): 国家自然科学基金项目(42192554,61827901); 中国气象科学研究院科技发展基金项目(2022KJ012);中国气象科学研究院基本科研业务费项目(2022Y006); 上海台风研究基金项目(TFJJ202210)资助~~
邮箱(Email): duanyh@cma.gov.cn;
DOI: 10.16441/j.cnki.hdxb.20240055
中文作者单位:

复旦大学大气与海洋科学系/大气科学研究院;中国气象科学研究院灾害天气国家重点实验室;

摘要(Abstract):

本文利用中国地面高时空分辨率的降水资料,分析台风“利奇马”(Lekima)登陆期间,其外雨带在浙江沿海地区产生的降水特征。结果表明,“利奇马”外雨带影响下浙江地区降水过程的累计降水、分钟雨强均呈现显著极端性,强降水中心呈现带状分布特征,在空间和时间上具有明显的非均匀性。同时,本次降水呈现出多种时间尺度的波动特征,周期128~192 min的波动信号贯穿了整个降水过程。外雨带主要位于台风移动方向前侧,其不同位置的降水波动特征有所不同,雨带外边缘降水小波功率谱有两个明显的大值中心,即除周期128~192 min波动信号外,还有准周期16~64 min的波动特征;雨带内侧则分为周期128~256 min的波动信号和多个周期在16 min以下的高频波动信号。本文的研究对提高登陆台风的降水精细化预测水平有重要意义。

关键词(KeyWords): 台风;利奇马;降水;时空演变;波动特征
参考文献

[1] 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.

[2] 李真真,吴立广,刘青元.近20a影响我国台风活动变化趋势[J].气象科学,2016,36(6):752-759.Li Z Z,Wu L G,Liu Q Y.Variation trend of typhoon activity influencing China during the past 20 years[J].Journal of the Meteorological Sciences,2016,36(6):752-759.

[3] 卢莹,赵海坤,赵丹,等.1984—2017年影响中国热带气旋灾害的时空特征分析[J].海洋学报,2021,43(6):1-17.Lu Y,Zhao H K,Zhao D,et al.Spatial-temporal characteristic of tropical cyclone disasters in China during 1984—2017[J].Acta Oceanologica Sinica,2021,43(6):1-17.

[4] 任福民,向纯怡.登陆热带气旋降水预报研究回顾与展望[J].海洋气象学报,2017,37(4):8-18.Ren F M,Xiang C Y.Review and prospect of researches on the prediction of precipitation associated with landfalling tropical cyclones[J].Journal of Marine Meteorology,2017,37(4):8-18.

[5] 陈联寿,孟智勇,丛春华.台风暴雨落区研究综述[J].海洋气象学报,2017,37(4):1-7.Chen L S,Meng Z Y,Cong C H.An overview on the research of typhoon rainfall distribution[J].Journal of Marine Meteorology,2017,37(4):1-7.

[6] Li Q Q,Wang Y Q.A comparison of inner and outer spiral rainbands in a numerically simulated tropical cyclone[J].Monthly Weather Review,2012,140:2782-2805.

[7] Kevin C,Yu Z F,Russell L E,et al.Recent advances in research and forecasting of tropical cyclone rainfall[J].Tropical Cyclone Research and Review,2018,72:106-127.

[8] Yang M J,Wu Y C,Liou Y C.The study of inland eyewall reformation of Typhoon Fanapi (2010) using numerical experiments and vorticity budget analysis[J].Journal of Geophysical Research:Atmospheres,2018,123(17):9604-9623.

[9] Corbosiero K L,Molinari J.The effects of vertical wind shear on the distribution of convection in tropical cyclones[J].Monthly Weather Review,2002,130(8):2110-2123.

[10] Corbosiero K L,Molinari J.The relationship between storm motion,vertical wind shear,and convective asymmetries in tropical cyclones[J].Journal of the Atmospheric Sciences,2003,60(2):366-376.

[11] Cecil,Daniel J.Satellite-derived rain rates in vertically sheared tropical cyclones[J].Geophysical Research Letters,2007,34(2):L02811.

[12] Ueno M.Observational analysis and numerical evaluation of the effects of vertical wind shear on the rainfall asymmetry in the typhoon inner-core region[J].Journal of the Meteorological Society of Japan Ser Ⅱ,2007,85(2):115-136.

[13] Zhou H B,Bai A J,Cai Q B.Analysis on asymmetric precipitation of the strong typhoon Nesat (1117) before and after landing on Hainan Island[J].Journal of Tropical Meteorology,2017,33(3):386-398.

[14] Yu Z F,Wang Y Q,Xu H M.Observed rainfall asymmetry in tropical cyclones making landfall over China[J].Journal of Applied Meteorology and Climatology,2015,54(1):117-136.

[15] Ouyang P,Wang Y Q,Zhang X N,et al.A numerical study of mesoscale-topography influence on the heavy rainband of typhoon Hato (2017)[J].Journal of Tropical Meteorology,2021,27(4):393-405.

[16] 陈涛,董林,罗玲,等.台风利奇马登陆期间的对流结构特征及对强降雨影响[J].气象,2021,47(12):1433-1443.Chen T,Dong L,Luo L Y,et al.Convection structure and impact on severe precipitation during landing of typhoon Lekima[J].Meteorology Monthly,2021,47(12):1433-1443.

[17] Yang S,Chen B,Zhang F,et al.Characteristics and causes of extremely persistent heavy rainfall of tropical cyclone In-Fa (2021)[J].Atmosphere,2022,13(3):398-419.

[18] Lu Y,Chen P Y,Yu H,et al.Parameterized tropical cyclone precipitation model for catastrophe risk assessment in China[J].Journal of Applied Meteorology and Climatology,2022,61(9):1291-1303.

[19] 陈宏,杨晓君,尉英华,等.干冷空气入侵台风“海棠”残余低压引发的华北地区大暴雨分析[J].暴雨灾害,2020,39(3):241-249.Chen H,Yang X J,Wei Y H,et al.Analysis of the heavy rain in North China for dry cold air intruding into typhoon "Begonia" depression[J].Torrential Rain and Disasters,2020,39(3):241-249.

[20] Meng W G,Wang Y.Adiagnostic study on heavy rainfall induced by typhoon Utor (2013) in South China:1.Rainfall asymmetry at landfall[J].Journal of Geophysical Research:Atmospheres,2016a,121(21):12781-12802.

[21] Meng W G,Wang Y.Adiagnostic study on heavy rainfall induced by landfalling typhoon Utor (2013) in South China:2.Postlandfall rainfall[J].Journal of Geophysical Research:Atmospheres,2016b,121(21):12803-12819.

[22] Deng D,Ritchie E A.Rainfallmechanisms for one of the wettest tropical cyclones on record in Australia-Oswald (2013)[J].Monthly Weather Review,2020,148(6):2503-2525.

[23] Lonfat M,Marks Jr F D,Chen S S.Precipitation distribution in tropical cyclones using the Tropical Rainfall Measuring Mission (TRMM) microwave imager:A global perspective[J].Monthly Weather Review,2004,132(7):1645-1660.

[24] Yu Z F,Wang Y Q,Xu H M,et al.On the relationship between intensity and rainfall distribution in tropical cyclones making landfall over China[J].Journal of Applied Meteorology and Climatology,2017,56(10):2883-2901.

[25] Wang Y Q.How do outer spiral rainbands affect tropical cyclone structure and intensity?[J].Journal of the Atmospheric Sciences,2009,66:1250-1273.

[26] 赵玉春,王叶红,陈健康,等.“莫兰蒂”台风 (2016) 登陆前后精细结构及其引发福建特大暴雨的模拟研究[J].暴雨灾害,2018,37(2):135-148.Zhao Y C,Wang Y H,Chen J K,et al.Numerical investigation on detailed structure of Typhoon "Meranti"(2016) and extreme heavy rainfall event induced by it before and after landfall in Fujian[J].Torrential Rain and Disasters,2018,37(2):135-148.

[27] 杨舒楠,曹勇,陈涛,等.台风苏迪罗登陆次日分散性暴雨成因及预报着眼点[J].气象,2019,45(1):38-49.Yang S N,Cao Y,Chen T,et al.Causes and focus points of forecasting the scattered rainstorm of typhoon Soudelor on Day 2 after landing[J].Meteorology Monthly,2019,45(1):38-49.

[28] Lin Y L,Li Y L,Li Q Q,et al.A long-lasting vortex Rossby wave-induced rainband of Typhoon Longwang(2005)[J].Bulletin of the American Meteorological Society,2018,99(6):1127-1134.

[29] Dai H N,Zhao K,Li Q Q,et al.Quasi-periodic intensification of convective asymmetries in the outer eyewall of typhoon Lekima(2019)[J].Geophysical Research Letters,2021,48(5):e2020GL091633.

[30] Huang H,Li Q Q,Zhao K,et al.Microphysical characteristics of the phase-locking VRW-induced asymmetric convection in the outer eyewall of Super Typhoon Lekima(2019)[J].Geophysical Research Letters,2022,49(9):e2021GL096869.

[31] Yu C K,Tsai C L.Surface pressure features of landfalling typhoon rainbands and their possible causes[J].Journal of the Atmospheric Sciences,2010,67(9):2893-2911.

[32] 王坚红,姜云雁,崔晓鹏,等.1956—2012年浙闽登陆热带气旋降水精细化观测统计分析[J].大气科学,2018,42(1):16-32.Wang J H,Jiang Y Y,Cui X P,et al.Statistical analysis of accurate observations of tropical cyclone precipitation in Zhejiang and Fujian Provinces from 1956 to 2012[J].Chinese Journal of Atmospheric Sciences,2018,42(1):16-32.

[33] 焦亚音,冉令坤,李娜,等.台风“彩虹” (2015) 高分辨数值模拟及涡旋Rossby波特征分析[J].物理学报,2017,66(8):37-47.Jiao Y Y,Ran L K,Li N,et al.High resolution numerical simulation of typhoon Mujigae (2015) and analysis of vortex Rossby waves[J].Acta Physica Sinica,2017,66(8):37-47.

[34] 周冠博,焦亚音,钱奇峰,等.1822号台风“山竹”的涡旋Rossby波特征分析[J].海洋气象学报,2020,40(3):37-47.Zhou G B,Jiao Y Y,Qian Q Q,et al.Analysis on characteristics of vortex Rossby wave in Typhoon Mangkhut (1822)[J].Journal of Marine Meteorology,2020,40(3):37-47.

[35] 薛一迪,崔晓鹏.“威马逊” (1409) 强降水物理过程模拟诊断研究[J].大气科学,2020,44(6):1320-1336.Xue Y D,Cui X P.Diagnostic and numerical study on physical process of strong rainfall associated with Rammasun(1409)[J].Chinese Journal of Atmospheric Sciences (in Chinese),2020,44(6):1320-1336.

[36] 谷欣蕊,罗亚丽,肖天贵,等.台风“苗柏”影响下局地强降水精细化垂直结构特征观测分析[J].成都信息工程大学学报,2022,37(3):290-301.Gu R X,Luo Y L,Xiao T G,et al.Observational analysis of the fine-scale vertical structure of localized heavy precipitation associated with typhoon “Merbok”[J].Journal of Chengdu University of Information Technology,2022,37(3):290-301.

[37] 胡鑫蓉.“黑格比”台风浙沪交界极端降水及物理量特征分析[J].热带气象学,2023,39(4):567-580.Hu X R.Analysis of extreme precipitation in the adjoining area of Zhejiang and Shanghai and physical quantity characteristics of typhoon Hagupit[J].Journal of Tropical Meteorology,2023,39(4):567-580.

[38] 向纯怡,赵海坤,刘青元,等.1909号台风“利奇马”登陆后强降水分布特征[J].气象科学,2020,40(3):294-302.Xiang C Y,Zhao H K,Liu Q Y,et al.The distribution of torrential rain after landfalling of typhoon “Lekima”(1909)[J].Journal of the Meteorological Sciences,2020,40(3):294-302.

[39] Willoughby H E,Marks Jr F D,Feinberg R J.Stationary and moving convective bands in hurricanes[J].Journal of the Atmospheric Sciences,1984,41(22):3189-3211.

[40] Gall R,Tuttle J,Hildebrand P.Small-scale spiral bands observed in Hurricanes Andrew,Hugo,and Erin[J].Monthly Weather Review,1998,126(7):1749-1766.

[41] Cecil D J,Zipser E J,Nesbitt S W.Reflectivity,ice scattering,and lightning characteristics of hurricane eyewalls and rainbands.Part Ⅰ:Quantitative Description[J].Monthly Weather Review,2002,130(4):769-784.

[42] Ryan B F,Barnes G M,Zipser E J.A wide rainband in a developing tropical cyclone[J].Monthly Weather Review,1992,120(3):431-447.

[43] Samsury C E,Zipser E J.Secondary wind maxima in hurricanes:Airflow and relationship to rainbands[J].Monthly Weather Review,1995,123(12):3502-3517.

[44] 张康波,冯明轩,雷德义.台风“利奇马”防御工作回顾[J].中国防汛抗旱,2019,29(11):1-3.Zhang K B,Feng M X,Lei D Y.Review of defense work of typhoon "Lekima"[J].China Flood & Drought Management,2019,29(11):1-3.

[45] 任芝花,张志富,孙超,等.全国自动气象站实时观测资料三级质量控制系统研制[J].气象,2015,41(10):1268-1277.Ren Z H,Zhang Z F,Sun C,et al.Development of three-step quality control system of real-time observation data from AWS in China[J].Meteorology Monthly,2015,41(10):1268-1277.

[46] 孙超,霍庆,任芝花,等.地面气象资料统计处理系统设计与实现[J].应用气象学报,2018,29(5):630-640.Sun C,Huo Q,Ren Z H,et al.Design and implementation of surface meteorological data statistical processing system[J].Journal of Applied Meteorological Science,2018,29(5):630-640.

[47] Jonathan D H,Xue M,Ran L K,et al.High-resolution modeling of typhoon Morakot (2009):Vortex Rossby waves and their role in extreme precipitation over Taiwan[J].Journal of the Atmospheric Sciences,2013,70(1):163-186.

[48] Li Y,Zhao D J.Climatology of tropical cyclone extreme rainfall over China from 1960 to 2019[J].Advances in Atmospheric Sciences,2022,39(2):320-332.

[49] 王晓,余晖,鲍旭炜,等.菲特 (1323) 台风降水的极端性分析[J].气象科学,2017,37(4) :514-521.Wang X,Yu H,Bao X W,et al.Analysis on extreme characteristics of the precipitation brought by typhoon “Fitow” (1323)[J].Journal of the Meteorological Sciences,2017,37(4):514-521.

[50] 孙虎林,黄焕卿,于庆龙,等.2012-2017年珠江口海区短时强对流天气灾害的统计分析[J].海洋预报.2019,36(4):35-43.Sun H L,Huang H Q,Yu Q L,et al.Statistical analysis of short-term severe convective weather disasters in the Pearl River Estuary during 2012—2017[J].Marine Forecasts,2019,36(4):35-43.

基本信息:

DOI:10.16441/j.cnki.hdxb.20240055

中图分类号:P426.6;P444

引用信息:

[1]彭成祥,端义宏,冯佳宁.2019年超强台风“利奇马”外雨带降水精细结构分析[J].中国海洋大学学报(自然科学版),2025,55(03):1-12.DOI:10.16441/j.cnki.hdxb.20240055.

基金信息:

国家自然科学基金项目(42192554,61827901); 中国气象科学研究院科技发展基金项目(2022KJ012);中国气象科学研究院基本科研业务费项目(2022Y006); 上海台风研究基金项目(TFJJ202210)资助~~

检 索 高级检索

引用

GB/T 7714-2015 格式引文
MLA格式引文
APA格式引文