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亚洲阻塞高压分类及其与东北冷涡活动和东北夏季低温的联系
  • ISSN号:1000-0690
  • 期刊名称:地理科学
  • 时间:2012.9
  • 页码:1269-1274
  • 分类:G42[文化科学—课程与教学论;文化科学—教育学;文化科学—教育技术学]
  • 作者机构:[1]中高纬度环流系统与东亚季风研究开放实验室,吉林长春130062, [2]吉林省气象服务中心,吉林长春130062, [3]吉林省气象科学研究所,吉林长春130062, [4]兰州大学,甘肃兰州730000
  • 相关基金:公益性行业(气象)科研专项(GYHY:201006020 201106016 201106015); 国家自然科学基金面上项目(41175083); 青年基金项目(40705036)资助
  • 相关项目:中国东北夏季低温前期征兆与北半球中高纬度海—气耦合过程变化的联系
中文摘要:

利用1948-2009年美国环境预报中心(NCEP)500 hPa高度场逐日再分析资料,按照通用的阻塞高压天气学定义,采用机器自动识别方法,检索和分析近62 a亚洲夏季阻高活动时空变化特征,结果表明:共统计到1 337个阻塞高压个例,以生命期3-7 d的过程居多,占80.1%,阻高活动累计个数和累计天数集中区可分为偏东类(鄂霍次克海)、偏西类(乌拉尔山)、中间类(贝加尔湖)和其他类4类,其中中间类阻塞高压活动累计个数最多,占总个数的30.4%,偏东类次之,占27.5%,其他类占23.8%,偏西类最弱,占18.3%;20世纪90年代以来,乌拉尔山地区阻高处于明显偏弱期,鄂霍次克海阻高处于偏强期;但是,21世纪初叶,乌拉尔山地区阻高活动开始呈上升趋势,而鄂霍次克海阻高却呈明显下降趋势,值得关注;夏季阻塞高压与东北冷涡活动天数呈显著同期正相关,与长春、哈尔滨同期平均气温呈显著负相关;亚洲夏季阻塞高压是影响东北夏季低温重要的环流系统;鄂霍次克海阻高6月活动异常年,850hPa风距平场在120°E-140°E,40°N-55°N存在很强的偏东气流,有利于来自鄂霍次克海偏东北路径的冷空气入侵东北亚及中国东北地区。

英文摘要:

Based on the daily NECP /NCAR reanalysis data of 500 hPa height field from 1948 to 2009,an objective classification and widely-agreed method was applied to analyze the temporal and spatial distributions of atmospheric blockings high in Asia during summer,In addition,the location and numbers of blockings high was automatically determined.The results show that there are 1 337 blocking events during the last 62 summers.According to the active period of blocking events,a period of 3-7 days are dominant during all the events which account for 80.1%.Based on the accumulative numbers and days,the blockings are divided into eastward type(blocking high over the Okhotsk Sea),westward type(blocking high over Ural Mountain),central type(blocking high over Baikal Lake) and the others,totally four types,occupying at 27.5%,30.4%,18.3%,and 23.8 %,respectively.Since 1990s,blocking events in Ural region are in a weak period,otherwise in Okhotsk region are in a strong period,but blocking events in Ural region begin taking upward trend at the beginning of 21st century.Bblockings in Okhotsk region take a clear downward trend.There is a significant positive relationship between blocking events and cold vortex in Northeast China,but a negative correlation between blocking events and temperature of Changchun and Harbin in summer.Blocking high is one of important circulation system which causes the low temperature in Northeast of China in summer.During westward type blocking events strongly active years in June,a strong easterlies air flow in 850 hPa is found over the region of 20°E-140°E,40°N-55°N,It is advantageous for cold air come from the northeast path in Okhotsk region to invade Northeast Asia and the northeast area in China.

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期刊信息
  • 《地理科学》
  • 北大核心期刊(2011版)
  • 主管单位:中科院
  • 主办单位:中国科学院 东北地理与农业生态研究所
  • 主编:陆大道
  • 地址:长春市高新北区盛北大街4888号
  • 邮编:130012
  • 邮箱:geoscien@iga.ac.cn
  • 电话:0431-85542212 85542217
  • 国际标准刊号:ISSN:1000-0690
  • 国内统一刊号:ISSN:22-1124/P
  • 邮发代号:8-31
  • 获奖情况:
  • 中国自然科学核心期刊,中国地理学会优秀地理期刊
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,荷兰文摘与引文数据库,美国剑桥科学文摘,日本日本科学技术振兴机构数据库,中国中国科技核心期刊,中国北大核心期刊(2004版),中国北大核心期刊(2008版),中国北大核心期刊(2011版),中国北大核心期刊(2014版),中国北大核心期刊(2000版)
  • 被引量:39183