引发黄山地区暴雨的台风特征分析OA
Analysis of the Characteristics of Typhoons Causing Heavy Rains in Huangshan Area
本文利用2007-2024年黄山地区185个自动气象站逐日降水常规气象资料及ERA5再分析数据,统计分析了引发该地区暴雨的台风特征.结果表明,(1)近18年来,引发黄山地区暴雨的台风平均每年有1.4个,其中2008年南部影响频次最高,达3个;发生时段主要集中在7-9月,影响时间一般为1~4 d,最长可达5 d;台风暴雨综合强度指数普遍为1~3和7,最强为20.(2)影响台风路径可分为5类,其中西北路径和偏北路径最多,近海路径次之,广东路径较少,偏西路径最少;不同路径下的台风暴雨综合强度指数差异明显,西北路径最强,偏北路径次之,广东路径和近海路径较弱,偏西路径影响最弱.(3)影响台风均伴有螺旋雨带,台风暖湿气团均与低层冷空气交汇,从而在台风路径的右前侧产生暴雨,多为台风本体降水,远距离降水较少;且台风本体降水结合黄山山脉地形作用产生的暴雨强度最强,尤其是对西北路径和偏北路径影响台风的暴雨增幅作用显著.
Based on daily precipitation data from 185 automatic meteorological stations and ERA5 reanalysis data in Huangshan area from 2007 to 2024,this study statistically analyzed the characteristics of typhoons causing heavy rainstorms in the heartland of Huangshan area.The analysis shows that the average number of typhoons that cause heavy rainstorms in Huangshan area is 1.4 per year,with the highest frequency of 3 occurring in 2008.These events are primarily concentrated from July to September,typically lasting 1 to 4 days and up to a maximum of 5 days.The comprehensive intensity index of typhoon-induced rainstorms generally ranges from 1 to 3,and 7,reaching a maximum of 20.The paths of typhoons affecting the region can be divided into five categories,among which the northwest and northward tracks are the most frequent,followed by the coastal track,with the Guangdong and westward tracks being the least frequent.The typhoon rainstorm intensity index varies significantly among different tracks,peaking for the northwest track,followed by the northward track,and reaching its lowest for the westward track.All affecting typhoons are accompanied by spiral rainbands.The convergence of the warm,moist air mass of the typhoon with low-level cold air predominantly generates heavy precipitation in the right-front quadrant of the typhoon's track.Precipitation is dominated by the typhoon's core circulation,whereas remote precipitation is relatively infrequent.Notably,the local topographic forcing of the Huangshan Mountains substantially amplifies the core precipitation intensity,particularly for typhoons following the northwest and northward tracks.
孙蓓蓓;方祥生;岳如画;刘裕禄;张景;范东福
黄山市气象局,安徽 黄山 245021黄山市气象局,安徽 黄山 245021黄山市气象局,安徽 黄山 245021黄山市气象局,安徽 黄山 245021黄山市气象局,安徽 黄山 245021歙县气象局,安徽 黄山 245200
天文与地球科学
台风暴雨时空分布台风路径特征分析黄山地区
typhoon rainstormspatiotemporal distributionfeature analysistyphoon pathHuangshan Mountain
《热带气象学报》 2026 (2)
221-231,11
国家自然科学基金项目(42106030)资助
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