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中国农学通报 ›› 2014, Vol. 30 ›› Issue (23): 218-223.doi: 10.11924/j.issn.1000-6850.2013-3211

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

甘南州2011年7月2—5日持续性暴雨天气成因分析

宁和平1,韩莹2,王建兵1,刘洪兰3   

  • 收稿日期:2013-12-09 修回日期:2014-01-13 出版日期:2014-08-15 发布日期:2014-08-15
  • 基金资助:
    甘肃省气象局 “甘肃省对流性天气预报预警系统建设” 项目。

Analysis of the Continuous Rainstorm in Gannan, Gansu Province, July 2-5, 2011

  • Received:2013-12-09 Revised:2014-01-13 Online:2014-08-15 Published:2014-08-15

摘要: 通过对2011年7月2日—5日甘南州出现的一次持续性暴雨天气过程成因的诊断分析,指出这次强降水天气过程与500 hPa上的切变线以及700 hPa强辐合区的位置密切相关。低层的强烈辐合为暴雨的发生、发展提供了动力条件。通过对物理量场的分析,发现这次持续暴雨过程中在中低层有明显的湿层及水汽的辐合,从而为降水提供了充足的水汽条件。在副高外围西南气流中的持续上升运动,源源不断地将水汽和能量向东输送到降水区,是形成这次持续性暴雨天气过程的主要原因。

关键词: 处理时间, 处理时间

Abstract: Diagnostic analysis was applied for a continuous rainstorm event in Gannan Gansu Province, July 2-5, 2011. The results demonstrated that: this rainfall event was related with the shear on 500 hPa and location of strong convergence zone on 700 hPa. Low-level strong convergence provided a favorable dynamic condition for the occurrence and evolvement of heavy rainstorm. Through the analysis of the physical field, it was found that during this continuous rainstorm, there existed an obvious moisture layer and convergence of water vapor in low-middle layer, thereby providing adequate moisture condition for precipitation. Rising in the southwest airflow movement around the periphery of subtropical high, the water vapor and energy were transported eastward to precipitation area, which was the main cause of the continuous rainstorm event.