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近30年夏季亚欧大陆中高纬度阻塞高压的统计特征
引用本文:李峰,丁一汇.近30年夏季亚欧大陆中高纬度阻塞高压的统计特征[J].气象学报,2004,62(3):347-354.
作者姓名:李峰  丁一汇
作者单位:1. 国家气象中心,北京,100081;南京气象学院,南京,210044
2. 国家气候中心,北京,100081
基金项目:国家科学技术部攀登A计划,南湾季风试验研究
摘    要:文中利用1970~2001年NCEP再分析500 hPa逐日高度场资料,根据阻塞高压的天气学定义,采用客观统计方法检索出近32 a亚欧中高纬度392个阻塞高压个例,对其进行了气候学分析.结果表明,亚欧中高纬地区夏季阻塞高压活动频繁,10 d以下的过程占绝对多数,地理分布主要集中在45~70°N之间,纬向上可划分5个高发区,其中乌拉尔山和贝加尔湖东部阻高活动频次最高,同时,每个区域中又存在着相应的阻高活跃区.亚欧中高纬地区夏季阻高活动具有明显的季节内变化特征.6月份,阻塞活动多发生在乌拉尔山地区和鄂霍次克海地区,以双阻为主要形势;7月份,欧洲区和贝加尔湖地区的阻塞活动有所增多,尤其贝加尔湖东部地区增多明显,而乌拉尔山地区的阻塞形势明显减少,鄂霍次克海地区的阻塞活动位置向北移动,多发生在60°N以北,双阻形势逐渐减弱,贝加尔湖地区的中阻形势有所增强.8月份,阻塞形势主要存在于贝加尔湖东西两区,中阻形势占据主导地位.亚欧中高纬地区夏季阻塞高压活动年际变化特征也很突出,且这种年际振荡有明显的地理差异.另外,研究表明亚洲北部的阻高活动多以稳定型为主,移动型阻高个例仅占6.6%.移动型阻高以起源于乌拉尔山地区最多,移距最长,生命期最长.偶极子类阻高多集中在贝加尔湖东部与乌拉尔山地区,约占该地区总阻高频次的62.0%和49.7%,平均生命期分别达到7 d/次和9 d/次以上.

关 键 词:阻塞高压  气候统计  时空分布
收稿时间:2003/11/6 0:00:00
修稿时间:2003年11月6日

STATISTICAL CHARACTERISTIC OF ATMOSPHERIC BLOCKING IN THE EURASIA HIGH-MID LATITUDES BASED ON RECENT 30-YEAR SUMMERS
Li Feng and Ding Yihui.STATISTICAL CHARACTERISTIC OF ATMOSPHERIC BLOCKING IN THE EURASIA HIGH-MID LATITUDES BASED ON RECENT 30-YEAR SUMMERS[J].Acta Meteorologica Sinica,2004,62(3):347-354.
Authors:Li Feng and Ding Yihui
Institution:National Meteorological Center, Beijing 100081;Nanjing Institate of Meteorology, Nanjing 210044;National Meteorological Center, Beijing 100081
Abstract:According to synoptic definition of blocking, a objective method is used to statistic atmospheric blocking in Eurasia high-mid latitudes based on 32-year summers by means of 1970-2001 NCEP analysis data. The results show that there are 392 blocking activities during period of past 32 summers. Blocking activity occur frequently in zone of 45-70°N, concentrate on five regions mainly, especially in Ural and the east part of Baikal. Most of them are less than 10 days. The feature of the blocking activity intra-seasonal variations is clear. Ural and Okhotsk are preferred areas for the blocking, occurring in form of double-blocking in Jun. the blocking activities increase in Baikal and Europe, particularly in the east part of Baikal, the activities decrease synchronously in Ural and they appear more frequently in North to 60°N in the Okhotsk area. Therefore, Mid-blocking pattern is more important in Jul. The change is more obvious, the mid-blocking that occur in Baikal is most remarkable in Aug.
Keywords:Atmospheric blocking  Statistic characteristic  Distribution of space-time  
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