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中国农学通报 ›› 2018, Vol. 34 ›› Issue (28): 106-113.doi: 10.11924/j.issn.1000-6850.casb18050011

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

浙江一次副高边缘强对流天气过程分析

刘力源,杨亦萍,高丽,黄晓龙   

  1. 台州市气象局,台州市气象局,台州市气象局,台州市气象局
  • 收稿日期:2018-05-03 修回日期:2018-07-06 接受日期:2018-07-13 出版日期:2018-10-11 发布日期:2018-10-11
  • 通讯作者: 刘力源
  • 基金资助:
    浙江省气象局预报员专项“台州市强对流天气指标研究”(2017YBY15);台州市科技局项目“台州新一代天气雷达产品的本地化研究” (2016A33386)。

A Severe Convective Process on the Edge of Subtropical High in Zhejiang

  • Received:2018-05-03 Revised:2018-07-06 Accepted:2018-07-13 Online:2018-10-11 Published:2018-10-11

摘要: 为进一步探究浙江强对流天气的成因,提升气象为农服务能力,利用常规观测资料、NCEP再分析资料及多普勒天气雷达资料等分析了2017 年8 月17 日浙江发生的一次大范围大风及冰雹天气过程,结果表明:(1)此次强对流天气过程产生于弱对流条件下,高空槽东移、西南气流增强改善了动力条件、热力条件和水汽条件,加强了不稳定层结;局地热对流、低层切变和地面辐合线为触发条件。(2)雷达垂直积分含水量密度是产生冰雹的一个重要指标,浙江本地VIL/ET≥3.9 时产生冰雹概率极大。(3)雷暴回波质心快速下降标志着大风天气的产生。雷暴后侧较干入流急流利于系统的发展加强,形成飑线。雷暴单体减弱后的大片层状降水回波长时间维持是强降水的主要成因。(4)大风天气爆发主要有2 个阶段,一是由飑线东移造成,二是飑线减弱后的单体风暴入海增强造成。飑线内部的弱中气旋是造成杭州湾沿岸大风的主要成因之一。飑线减弱后入海增强可能为海陆热力性质差异导致。

关键词: 腐殖酸钾, 腐殖酸钾, 烤烟, 红花大金元, 品质, 影响

Abstract: Exploring the cause of strong convective weather in Zhejiang will improve meteorological service for agricultural production. In this paper, the conventional observation data, NCEP reanalysis data and Doppler weather radar data were used to analyze widespread gale and a hail weather process occurred in Zhejiang on August 17, 2017. The results showed that: (1) the strong convection weather process generated under the condition of weak convection, with the eastward and southwest airflow of the high groove increasing, the dynamic conditions, thermal conditions and water vapor conditions were improved, and the unstable stratification was strengthened, local geothermal convection, low-level shear and ground convergence were the trigger condition; (2) vertically integrated water content density was an important radar indicator of the hail, in addition, the hail probability was very high when the local VIL/ET≥3.9 in Zhejiang; (3) the rapid drop of the echo centroid of thunderstorm indicated the occurrence of the gale weather, the dry inflow jet behind the thunderstorm was conducive to the development of the system and the formation of squall lines, long-time maintenance of large stratiform precipitation echoes after the decrease of thunderstorm was the main cause of heavy rainfall; (4) there were two main stages of gale weather, one was caused by the eastward movement of squall line and the other was the increase of single storm after squall line weakening, the weak mesocyclone inside the squall line was one of the main causes of the gale along the Hangzhou Bay coast, the increase of storms into the sea might be caused by the difference of thermal properties between sea and land.