| 豫北一次局地雹暴天气的预警特征和触发机制 |
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| 引用本文： | 苏爱芳,梁俊平,崔丽曼,刘超.豫北一次局地雹暴天气的预警特征和触发机制[J].气象与环境学报,2012,28(6):1-7. |
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| 作者姓名： | 苏爱芳 梁俊平 崔丽曼 刘超 |
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| 作者单位： | 1.河南省气象台，河南 郑州 450003；2.河南省(中国气象局)农业气象保障与应用技术重点实验室，河南 郑州 450003 |
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| 基金项目： | 公益性行业(气象)科研专项 |
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| 摘 要： | 利用常规气象观测、多普勒雷达、卫星资料和区域自动站观测资料及NCEP再分析资料，对2011年6月11日豫北局地强对流天气的预报预警特征和触发机制进行分析。结果表明：局地强对流天气是在东北冷涡背景下产生的，高低层中尺度影响系统(槽、切变线、大风速轴)交汇处右侧是强对流发生潜势区。局地强对流天气发生前，CAPE较大，0-6 km垂直风切变达到中等偏强，有利于超级单体的形成和发展。高空冷平流南侵、低层暖平流北上，有利于大气对流不稳定度进一步加大。中-β尺度强对流云团在东北冷涡槽底后部形成，其发展演变对局地强对流天气预报预警有参考意义。强对流回波经历了细胞状、带状发展期和块状减弱期。回波带南侧形成的超级单体造成了局地强风雹天气，冰雹发生时伴有“三体散射”现象。冷空气和地面辐合线是强对流天气的主要触发机制；地面辐合线对强对流天气还有提示作用。
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| 关 键 词： | 局地冰雹 订正探空 超级单体 BWER 地面辐合线 局地冰雹 订正探空资料 超级单体 BWER 地面辐合线 触发机制 |
Warning characteristic and trigger mechanism of a local strong hailstorm in northern He'nan province |
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| SU Ai-fang,LIANG Jun-pin,CUI Li-man,LIU Chao.Warning characteristic and trigger mechanism of a local strong hailstorm in northern He'nan province[J].Journal of Meteorology and Environment,2012,28(6):1-7. |
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| Authors: | SU Ai-fang LIANG Jun-pin CUI Li-man LIU Chao |
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| Institution: | 1. He’nan Provincial Meteorological Observatory, Zhengzhou 450003, China; 2. Key Laboratory of Agrometeorological Ensuring and Applied Technique, China Meteorological Administration, Zhengzhou 450003, China |
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| Abstract: | Based on the conventionally meteorological observation data, Doppler radar data, satellite data, meteoro- logical data from regional automatic weather stations and the NCEP reanalysis data, the forewarning characteristic and trigger mechanism of a local strong hailstorm occurred on June 11,2011 in the northern He＇nan province were analyzed. The results show that the local severe convective weather occurs under the background of the northeast cold vortex, and the potential area of severe convective weather is located on the fight side of the junction areas of upper and lower mesoscale synoptic system（ trough, sheer line, the axis of larger wind speed）. The CAPE values are large and the vertical wind sheer from 0 km to 6 krn determined from the revised sounding data before the local severe hailstorm weather happens is moderate or strong, which facilitate the formation and development of super- cell. The convective instability of atmosphere increases while the cold advection in upper level moves southward and the warm advection in lower level moves northward. The meso-fl-scale convective cloud cluster is generated in the rear of the northeast cold vortex and its development and evolution have some certain reference values for weather warning. Strong convective echo goes through the developing stage with cell shape to band shape and the weakening stage with block shape. The supercell generated on the south of the convective echo-belt results in the characteristic of ＇three-body scattering＇ when the local severe hailstorm weather appears. The cold air and surface convergence lines are the important trigger mechanisms for severe convective weather, and the surface convergence lines are indicative for strong convection weather. |
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| Keywords: | Local hailstorm Revised radiosonde data Supercell Bounded weak echo region (BWER) Surfaceconvergence lines Trigger mechanism |
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