干旱气象 ›› 2021, Vol. 39 ›› Issue (4): 620-630.

• 论文 • 上一篇    下一篇

陕西汉中及其周边地区对流活动的雷达气候特征分析

支树林1,许东蓓2,潘赫拉3,李典南4,包慧濛1,陈娟1   

  1. (1.江西省气象台,江西南昌330096;2.成都信息工程大学大气科学学院,四川 成都610225;
    3.中国人民解放军陆军航空兵学院,北京101123;4.贵州省气象台,贵州 贵阳550002)


  • 出版日期:2021-08-31 发布日期:2021-09-13
  • 作者简介:支树林(1976― ),男,江苏宝应人,正高级工程师,主要从事短临预报相关研究. E-mail: zhisl00@126.com。
  • 基金资助:
    国家自然科学基金重点项目(91937301)和江西省气象局项目(JX2020Z02和JX2020M02)共同资助

Analysis on Radar Climatic Characteristics of Convective Activities in and Around Hanzhong Areas in Shaanxi Province

ZHI Shulin1, XU Dongbei2, PAN Hela3, LI Diannan4,BAO Huimeng1, CHEN Juan1   

  1. (1. Jiangxi Meteorological Observatory, Nanchang 330096, China;
    2. School of Amospheric Sciences, Chengdu University of Information Technology, Chengdu 610225, China;
    3. Chinese People’s Liberation Army Aviation School, Beijing 101123, China;
    4. Guizhou Meteorological Observatory, Guiyang 550002, China)

  • Online:2021-08-31 Published:2021-09-13

摘要: 利用2013—2017年6—8月汉中雷达资料,基于等高平面位置显示(constant altitude plan position indicator, CAPPI)上的对流区判识结果,统计分析汉中及其周边地区暖季对流活动气候特征,发现该地区对流活动高发地主要位于大巴山区、秦岭东南麓和汉中以东的秦岭大巴山过渡带,其中大巴山的对流频数最高、较高频数的区域也最广,秦岭东南麓及大巴山过渡带次之,汉中盆地西部对流频数最少。7月对流活动最频繁,6月最少,对流频数及面积也呈明显的日变化特征。对流高发区位置与山地地形特征高相关:大巴山区对流频数高值区与地形高处接近重合,秦岭东南麓的高值区则位于山坡处。对流伸展高度基本都在7 km以下,其中4~5 km高度占比最高。基于再分析资料的分析发现,7—8月,四川盆地东部维持CAPE高值中心,其位置与四川盆地北侧的大巴山区非常接近,这也是大巴山区持续为对流频数高值中心的可能原因之一。

关键词: C波段雷达, 对流频数, 秦岭, 大巴山区, 对比

Abstract: Based on the radar data in Hanzhong from June to August during 2013-2017 and the convective zone on constant altitude plan position indicator by using discrimination method, the characteristics of convective activities were analyzed during the warm season in and around Hanzhong areas. The results show that the high frequency areas of convective activities were mainly located in the Daba mountains, the southeastern foothills of the Qinling mountains and the transitional zone of the eastern QinlingDaba mountains around Hanzhong city, the highest convective frequencies and the widest areas were in the Daba mountains, followed by the southeastern foot of the Qinling mountains and the transitional zone of the Qinling and Daba mountains, and convective frequency was least in the western part of the Hanzhong basin. The convective activity was most in July and least in June, and convective frequency and convective areas showed obvious diurnal variation. The locations of convective high frequencies areas were highly correlated with mountainous terrain features. The high convection frequencies areas in the Daba mountains nearly coincided with terrain heights, while the high value areas in the southeastern foothills of the Qinling mountains were located on mountain slopes. The convection extension height was mostly below 7 km, with the highest proportion at a height of 4 to 5 km. Based on the reanalysis data, it was found that the convective instability energy maintained a high value center in the eastern part of the Sichuan basin in July and August, which was very close to the Daba mountains in the north of it, and it may be one of the contributing factors to the persistence of the local high convective region.


Key words: Key words: C-band radar, convection frequency, the Qinling mountains, the Daba mountains area, comparison

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