欢迎您！东篱公司
退出
-
申报数据库
-
立项数据库
-
成果数据库
-
项目获奖数据库
中文摘要：
受1522号台风彩虹外围螺旋云带影响,2015年10月4日15时28分—16时（北京时）广东佛山出现了EF3级强龙卷并造成严重灾害。为了综合分析龙卷发生的多尺度环境背景场和龙卷的结构及强度变化等特点,进行了灾情调研,航拍龙卷灾情路径,走访龙卷目击者,确认龙卷路径及灾情级别,再结合多渠道获取的龙卷视频照片等资料以及观测资料进行分析研究,结果表明：（1）产生此次龙卷的超级单体存在于台风彩虹外围螺旋云带内;龙卷向西北偏北方向移动,触地时长为32 min,受灾路径长度为31.7 km,最大受灾直径为577 m,平均速度约为60 km/h,具有＂移动速度快,影响范围广,破坏力强＂的特点,其移动速度快慢似与超级单体强度和地面的粗糙度有关。（2）佛山地区中高层受偏南气流控制,水汽充足,地面有弱冷空气;珠三角喇叭口地形有利于气流的辐合与局地涡旋的产生;抬升凝结高度低,风垂直切变大,有利于龙卷的生成。（3）地面自动气象站气象要素表现出受龙卷环流影响的特征。3 s极大风速的大值带和3 s最低气压的低值带以及1 h累计降水大值中心呈现出与龙卷走向一致的东南—西北向带状分布;龙卷到来时其周围自动气象站气温和气压明显降低,风速明显增大,风向明显改变;降水在龙卷靠近前5—10分钟就开始明显增大,其大值中心位于龙卷路径的西侧。龙卷离开后气压比龙卷来临前有所升高,但气温较前降低。（4）龙卷出现在钩状回波前进方向的右后侧;降水大值区与雷达组合反射率大值区基本一致。地面风场的辐合中心与龙卷触地的位置基本一致,并且钩状回波的入流区与地面偏东风区相对应。龙卷风暴单体发展高度在4 km左右,具有低重心对流的特点。其前部存在回波悬垂,一条很窄的向西北倾斜的回波大值带可能与龙卷漏斗云墙有关。对应径向速度剖面图上为一?
英文摘要：
A tornado, rated as a category 3 storm on the enhanced Fujita scale （EF3）, occurred at Foshan as part of Typhoon ＂Mujigae＂ （2015） between 15：28 BT and 16：00 BT 4 October 2015. This tornado lasted for 32 rain and destroyed a large num- ber of factories and houses. The tornado swath was about 31. 7 km, and the largest tornado swath diameter reached up to 577 m. Photos and tornado videos were collected in the survey of damages caused by the tornado. In addition, the surface auto- matic weather station data, regular observational data, and Doppler radar data were used in this paper to analyze this tornado process. The tornado life cycle was divided into three stages： The developing stage, the mature stage, and the dissipating stage. The tornado moved faster in the developing and mature stage than in the dissipating stage when it slowed down due to changes in the intensity of the supercell and surface roughness. The large scale circulation featured by obvious wind shear and high moisture in the lower levels was favorable for the tornado genesis. Cold air extended to the south as the small trough stretched southward in the surface layer, high SWEAT index, high K index and low lifting condensation level （LCL） were found in the unstable layer. These were necessary environmental conditions for tornado genesis. The bell shape terrain of the Pearl River Delta region is also favorable for the development of convergence and local vortex genesis in the surface layer. The variables recorded by the surface automatic weather stations showed strong signals when the tornado passed by. The distribu- tion of 3 s gust and 3 s minimum pressure extended along the northwest--southeast direction, which was consistent with the tornado swath. The pressure and temperature dropped sharply while the wind speed increased dramatically during the tornado development period, and cyclonic convergent winds circled around the tornado. The rainfall started to increase 5 to 10 rain be- fore the tornado arrived, and the main rainfa
同期刊论文项目
同项目期刊论文
期刊信息
位置：