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不同路径台风影响舟山的大风气候特征分析
作者:朱思瑜  陈淑琴  方言 
单位:舟山市气象局, 浙江 舟山 316021
关键词:舟山 台风大风 台风路径 点聚图 
分类号:P444
出版年·卷·期(页码):2024·41·第五期(119-125)
摘要:
将台风路径分为在浙江登陆的台风、在福建及以南登陆的台风、海上转向台风、在浙江以北登陆的台风这4种分别研究舟山的台风大风特征。4种台风路径中影响舟山最多的为海上转向台风,其中在125°E转向的最多,最少的为在浙江以北登陆的台风。统计分析1989—2020年4种不同路径台风影响舟山过程风力的分布范围、中位数、极大值等气候特征,并研究不同路径下台风过程风力与台风中心和舟山的最近距离以及最近距离时的台风强度之间的分布关系,以此绘制点聚图。
This paper divides typhoon paths into four types to study the climatic gale characteristics in Zhoushan: typhoons that landed in Zhejiang, typhoons that landed in or south of Fujian, typhoons that turned offshore, typhoons that landed north of Zhejiang. Typhoons which have the largest impacts on Zhoushan is those turned offshore, while typhoons which have the smallest impacts on Zhoushan is those landed north of Zhejiang. It is found that typhoons that turned offshore mostly turned at 125°E. This study further analyzes the climatic wind characteristics during the typhoon processes affecting Zhoushan from 1989 to 2020, such as distribution areas, median value, and maximum value. The relationships among wind grade, typhoon intensity and the closest distance between the typhoon center and Zhoushan are also studied.
参考文献:
[1] WEBSTER P J, HOLLAND G J, CURRY J A, et al. Changes in tropical cyclone number, duration, and intensity in a warming environment[J]. Science, 2005, 309(5742):1844-1846.
[2] EMANUEL K. Increasing destructiveness of tropical cyclones over the past 30 years[J]. Nature, 2005, 436(7051):686-688.
[3] 陈联寿, 丁一汇. 西太平洋台风概论[M]. 北京:科学出版社, 1979:440-448. CHEN L S, DING Y H. Introduction to the western Pacific typhoon [M]. Beijing:Science Press, 1979:440-448.
[4] 田辉, 马开玉, 林振山. 华南、华东沿海登陆台风暴雨和大风的分析[J]. 应用气象学报, 1999, 10(S1):148-152. TIAN H, MA K Y, LIN Z S. Analysis of the heavy rain and strong wind of landing typhoon on the coasts of south and east China[J]. Journal of Applied Meteorological Science, 1999, 10(S1):148-152.
[5] 李英, 陈联寿, 张胜军. 登陆我国热带气旋的统计特征[J]. 热带气象学报, 2004, 20(1):14-22. LI Y, CHEN L S, ZHANG S J. Statistical characteristics of tropical cyclone making landfalls on China[J]. Journal of Tropical Meteorology, 2004, 20(1):14-22.
[6] 程正泉, 陈联寿, 刘燕, 等. 1960—2003年我国热带气旋降水的时空分布特征[J]. 应用气象学报, 2007, 18(4):427-434. CHENG Z Q, CHEN L S, LIU Y, et al. The spatial and temporal characteristics of tropical cyclone-induced rainfall in China during 1960—2003[J]. Journal of Applied Meteorological Science, 2007, 18(4):427-434.
[7] 周惠文, 陈冰廉, 苏兆达, 等. 广西台风灾害性大风的气候特征[J]. 灾害学, 2007, 22(1):13-17. ZHOU H W, CHEN B L, SU Z D, et al. Characteristics of disastrous gale in Guangxi[J]. Journal of Catastrophology, 2007, 22(1):13-17.
[8] 杨玉华, 雷小途. 我国登陆台风引起的大风分布特征的初步分析[J]. 热带气象学报, 2004, 20(6):633-642. YANG Y H, LEI X T. Statistics of strong wind distribution caused by landfall typhoon in China[J]. Journal of Tropical Meteorology, 2004, 20(6):633-642.
[9] 钮学新, 朱持则. 热带气旋大风圈的预报[J]. 热带气象学报, 1997, 13(4):365-367. NIU X X, ZHU C Z. The forecast of wind circles in tropical cyclone[J]. Journal of Tropical Meteorology, 1997, 13(4):365-367.
[10] 陈润珍, 孔宁谦. 广西沿海热带气旋大风数值预报探讨[J]. 海洋预报, 2004, 21(1):52-55. CHEN R Z, KONG N Q. Research of numerical forecast of tropical-cyclone gale in littoral of Guangxi[J]. Marine Forecasts, 2004, 21(1):52-55.
[11] 王雷, 李晓丽, 徐哲永. 近50年影响舟山的台风气候特征分析[J]. 海洋预报, 2011, 28(5):36-43. WANG L, LI X L, XU Z Y. Analysis on climatic characteristics of typhoon over the past 50 years at Zhoushan[J]. Marine Forecasts, 2011, 28(5):36-43.
[12] 梁莉, 崔晓鹏, 王成鑫, 等. 我国登陆热带气旋引起的大陆地面风场分布[J]. 大气科学, 2018, 42(1):96-108. LIANG L, CUI X P, WANG C X, et al. Characteristic distribution of surface winds associated with landfalling tropical cyclones in China's mainland[J]. Chinese Journal of Atmospheric Sciences, 2018, 42(1):96-108.
[13] 曹楚, 王忠东, 郑峰. 台风“莫拉克”影响期间浙江大风成因分析[J]. 气象科技, 2013, 41(6):1109-1115. CAO C, WANG Z D, ZHENG F. Causal analysis of strong wind weather in Zhejiang induced by typhoon "Morakot" [J]. Meteorological Science and Technology, 2013, 41(6):1109-1115.
[14] 王忠东, 曹楚, 楼丽银, 等. 超强台风“罗莎”和“韦帕”大风过程对比分析[J]. 气象科技, 2009, 37(2):156-161. WANG Z D, CAO C, LOU L Y, et al. Comparative analysis of high wind processes in super typhoon "Krosa" and "Wipha" [J]. Meteorological Science and Technology, 2009, 37(2):156-161.
[15] 王亚男, 王庆元. 1210号台风大风和渤海湾天津沿岸风暴潮分析[J]. 海洋预报, 2013, 30(6):7-12. WANG Y N, WANG Q Y. Analysis of No.1210 typhoon gale and storm surge along Tianjin coast of the Bohai Bay[J]. Marine forecasts, 2013, 30(6):7-12.
[16] 陈德花, 张玲, 张伟, 等.“莫兰蒂”台风致灾大风的结构特征及成因[J]. 大气科学学报, 2018, 41(5):692-701. CHEN D H, ZHANG L, ZHANG W, et al. Structure characteristics and cause analysis of catastrophic wind caused by super typhoon "Meranti"[J]. Transactions of Atmospheric Sciences, 2018, 41(5):692-701.
[17] 李君, 李妍, 贾瑞, 等. 两个相似路径台风引发的东部沿海地区降水分布特征及成因对比分析[J]. 海洋预报, 2022, 39(3):25-36. LI J, LI Y, JIA R, et al. A comparison analysis of precipitation distribution over the eastern coastal area and their causes between two typhoons with similar paths[J]. Marine Forecasts, 2022, 39(3):25-36.
[18] 董美莹, 俞燎霓.“麦莎”台风影响期间浙江的大风分布特征和成因分析[J]. 科技导报, 2006, 24(4):29-32. DONG M Y, YU L N. Study on Matsa's gale characteristics occurred in Zhejiang province and their formation[J]. Science & Technology Review, 2006, 24(4):29-32.
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