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中国农学通报 ›› 2017, Vol. 33 ›› Issue (7): 148-152.doi: 10.11924/j.issn.1000-6850.casb16100104

所属专题: 农业气象

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

陇东暖区切变暴雨特征及成因分析

李祥科,焦美龄,路亚奇,张洪芬   

  1. 甘肃省庆阳市气象局 745000,甘肃省庆阳市气象局 745000,甘肃省庆阳市气象局 745000,甘肃省庆阳市气象局 745000
  • 收稿日期:2016-10-25 修回日期:2016-12-14 接受日期:2016-12-19 出版日期:2017-03-16 发布日期:2017-03-16
  • 通讯作者: 李祥科
  • 基金资助:
    甘肃省气象局“陇东暖区切变暴雨特征及成因分析”(2015-06)

Warm Area’s Shear Rainstorm in Eastern Gansu: Characteristic Analysis

  • Received:2016-10-25 Revised:2016-12-14 Accepted:2016-12-19 Online:2017-03-16 Published:2017-03-16

摘要: 为了更好的做好对暴雨灾害预报分析能力,减少暴雨灾害对农业及人们生产生活的影响,笔者利用庆阳市2007—2014年8年间发生的暖区切变暴雨的地面及高低空资料,对其时空分布特征、影响因素及成因进行分析。结果表明:庆阳市暖区切变暴雨受温湿条件影响较大,暴雨多发生在地理条件适宜、湿度条件较好的宁县西部、庆城与合水交界处、华池中西部、环县南部及镇原东部的区域;对比陇东暴雨多发的4—9 月,暖区切变暴雨主要集中在7—8 月,以7 月下旬和8 月下旬最多,占发生总数的85.7%;庆阳市暖区切变暴雨的发生前为持续性偏南风,时间长达3~7 天,相对湿度和温度会有1 个明显的跃变,在T-logP 图上反映出有较强的不稳定能量,Cape 值较大;落区主要是受地形影响和中层的干侵入有关,不确定性较强,切变线附近及其两侧都有发生;触发系统主要为暖式切变线,可分为低涡型和西南气流型。

关键词: 高温, 高温, ‘巨玫瑰’, 叶片表型, 可溶性糖, 叶绿素荧光

Abstract: To improve the ability of forecasting and analyzing the rainstorm disaster, reduce the impact of rainstorm disaster on agriculture and people’s life and production, by using the data of warm area’s shear rainstorm on the ground and high altitude in Qingyang from 2007 to 2014, the authors analyzed the spatial and temporal distribution characteristics, influencing factors and causes of warm area’s shear rainstorm. The results showed that: temperature and humidity conditions had significant influence on the warm area’s shear rainstorm in Qingyang, usually the rainstorm occurred in the western Ning county, the junction of Qingcheng and Heshui, mid- western Huaci and southern Huan county and eastern Zhenyuan, which had suitable geographical and humidity conditions; contrasting with rainstorm in eastern Gansu happening in April to September, warm area’s shear rainstorm mainly concentrated in July and August, 85.7% of them happened in late July and late August; persistent southerly winds could last 3-7 days before warm area’s shear rainstorm in Qingyang, there would be an obvious jump on relative humidity and temperature; the strong instability energy was reflected on the T- logP chart and the Cape value was relatively big; falling area was mainly affected by topography and middle dry intrusion, with strong uncertainty, and happened near the shear line on both sides; the trigger system was mainly the warm shear line, it could be divided into the vortex type and southwest airflow type.