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气象:2019,45(6):777-790
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珠江三角洲台风龙卷的活动特征及环境条件分析
黄先香,俞小鼎,炎利军,李彩玲,李兆明
(佛山市龙卷风研究中心,广东佛山 528000; 中国气象科学研究院灾害天气国家重点实验室,北京 100081; 中国气象局气象干部培训学院,北京 100081)
Analysis of Typhoon-Tornado Activity Characteristics and Environmental Condition in the Pearl River Delta
HUANG Xianxiang,YU Xiaoding,YAN Lijun,LI Cailing,LI Zhaoming
(Foshan Tornado Research Center of Guangdong Province, Foshan 528000; State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences, Beijing 100081; China Meteorological Administration Training Centre, Beijing 100081)
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投稿时间:2018-04-16    修订日期:2018-08-06
中文摘要: 利用常规观测、自动气象站、多普勒雷达等资料分析珠江三角洲台风龙卷的活动特征及其产生的环境条件。结果表明:台风龙卷发生在6—10月,时间多为10—20时,出现在台风登陆后1.3~21.3 h的时段内;多数龙卷位于台风中心的东北象限,台风中心在广东湛江—广西东南部或北部湾附近时是珠江三角洲龙卷发生的高风险期。高层辐散、低层辐合及中低空强东南急流在珠江口附近叠加是龙卷产生的有利环流背景。强或弱龙卷环境条件的共同特征为低抬升凝结高度、强深层和低层垂直风切变及较大风暴相对螺旋度(SRH),主要差异是强龙卷的深层和低层垂直风切变与SRH更大;相似台风路径下,有/无龙卷环境条件的明显差异在于0~1 km低层垂直风切变和SRH,两值越大出现超级单体或中气旋的可能性越大,龙卷发生概率也就越高。台风龙卷风暴母体属于低质心的微型超级单体风暴;低层有强或中等强度中气旋,有时强中气旋中心伴有龙卷涡旋特征(TVS);龙卷出现在钩状回波顶端或TVS附近。与西风带超级单体龙卷相比,台风龙卷中气旋的尺度更小、垂直伸展高度更低。
Abstract:Based on the data of conventional observation, automatic weather station and Doppler weather radar, this paper analyzes the activity characteristics and environmental condition of the typhoon-tornadoes in the Pearl River Delta. The results show that tornadoes occur from June to October and the time is concentrated in the period from 10:00 BT to 20:00 BT. Tornadoes occur between 1.3 h and 21.3 h after typhoon landfall. A strong preference for tornado occurrence is in the northeast quadrant with respect to land-falling typhoon center. High risk periods of tornado genesis in the Pearl River Delta correspond to the typhoon center locating between Zhanjiang of Guangdong and southeast Guangxi or Beibu Gulf. The synoptic situation of upper-level divergence, low-level convergence, and superimposition of strong southeasterly jets at mid- and low-layer over the Pearl River Delta are conducive to the weather background of tornadoes. The common environmental conditions for strong or weak tornado genesis appear to be low LCL, strong deep-layer and low-level vertical wind shear (VWS) and high storm relative helicity (SRH). The major difference between weak and strong tornado cases is that the latter has stronger deep-layer and low-level VWS and greater SRH. The significant diversities are VWS at 0-1 km and SRH between tornadic and nontornadic environmental conditions under the similar typhoon tracks. With the higher values of VWS and SRH, the possibility of supercells and mesocyclones increases, thus tornadoes are most likely to be detected. Tornado storms are mini supercell storms with low centriod. Strong or moderate mesocyclones are likely to be detected through the radial velocity data of the CINRAD/SA radar at low level, and significant tornadic vortex signature (TVS) may be found in the center of mesocyclones. The tornadoes lie in the interior of the hook echo or near TVS. Compared with the supercell tornadoes in the westerlies, mesocyclones of typhoon tornadoes are smaller in scale and lower in stretching height.
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基金项目:国家自然科学基金项目(41175043和41675023)、广东省科技厅社会发展科技协同创新体系建设专项(2019B020208015)、灾害天气国家重点实验室开放课题(2018LASW-B18)共同资助
引用文本:
黄先香,俞小鼎,炎利军,李彩玲,李兆明,2019.珠江三角洲台风龙卷的活动特征及环境条件分析[J].气象,45(6):777-790.
HUANG Xianxiang,YU Xiaoding,YAN Lijun,LI Cailing,LI Zhaoming,2019.Analysis of Typhoon-Tornado Activity Characteristics and Environmental Condition in the Pearl River Delta[J].Meteor Mon,45(6):777-790.