欢迎访问《中国农学通报》,

中国农学通报 ›› 2016, Vol. 32 ›› Issue (23): 113-121.doi: 10.11924/j.issn.1000-6850.casb16010058

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

2013年山西5次典型强对流天气分析

赵桂香,闫慧,董文晓   

  1. 山西省气象台,山西省气象台,山西省气象台
  • 收稿日期:2016-01-13 修回日期:2016-02-22 接受日期:2016-02-24 出版日期:2016-08-10 发布日期:2016-08-10
  • 通讯作者: 赵桂香
  • 基金资助:
    国家自然科学基金项目“黄河中游地区突发性大暴雨MCC结构特征研究”(41475050);山西省气象局课题“山西夏季冰雹天气特征对比及预警指标研究”(SXKYBTQ201510019)。

5 Typical Strong Convective Weather Processes in Shanxi in 2013

  • Received:2016-01-13 Revised:2016-02-22 Accepted:2016-02-24 Online:2016-08-10 Published:2016-08-10

摘要: 为了更好地为农业生产预防冰雹、减少灾害损失提供有效的气象预报服务,本研究利用多种气象观测资料,对2013年5次典型强对流天气进行了综合分析。结果表明:(1)冰雹发生在高能、高湿以及较强抬升条件的有利天气背景下,大尺度强迫抬升、低层中尺度露点锋和地面辐合线是强对流天气的重要触发机制。(2)冰雹极易发生在午后SI明显减小,Ki指数、500 hPa与850 hPa温差以及CAPE明显增大,同时垂直风切变较大、0℃和-20℃层高度分别在600 hPa和400 hPa左右的情况下,湿度条件较好时会伴随短时强降水天气,强气流控制下常伴随雷暴大风。(3)冰雹常出现在对流云团成熟时、TBB等值线梯度最大值东南侧,且组合反射率因子强度>55 dBZ的对流单体内。(4)地面温度异常变化、气压梯度较大、风向顺时针旋转及风速极值同时出现可视为强对流天气发生前的一种信号。

关键词: 油茶, 油茶, 嫁接苗, 施氮浓度

Abstract: In order to provide effective weather forecast service for the agricultural production to prevent hail and reduce disaster losses and do the hail weather forecast well. Five typical strong convective weather processes in 2013 had been comparison and analysis in this paper by using various meteorological observation data. The results show that: (1) The hail occurred under advantageous synoptic background such as high volatile energy, big humidity and strong lifting condition. The large-scale forced uplift, lower meso-scale dew point front, and the ground convergence line were provided the trigger conditions for the strong convection weather. (2) The hail easily happened in the case of SI having decreased obviously, Ki (K index), the temperature difference between 850 hPa and 500 hPa and CAPE increased obviously in the afternoon, meanwhile having the large vertical wind shear, and also the height of 0℃ and -20℃ layer at about 600 hPa and 400 hPa respectively. In addition, bigger humidity was accompanied by short-time strong rainfall weather and strong airflow was often accompanied by thunderstorm and wind. (3) The hail usually occurred when the convective clouds reached maturity, in the southeast of the maximum gradient of TBB (Black Body Temperature) contour, and in the convective cells of the maximum radar reflectivity factor was bigger than 55 dBZ. (4) If the temperature in the ground occurred abnormal changes, at the same time, there were bigger pressure gradient, clockwise rotation of wind direction, and wind speed extreme, it can be considered as a signal before the strong convective weather happened.