吉林省气象台, 吉林市气象台. 1981: 100毫巴极涡和南亚高压的活动与东北区夏季低温的关系. 气象学报, (4): 483-494. DOI: 10.11676/qxxb1981.052
引用本文: 吉林省气象台, 吉林市气象台. 1981: 100毫巴极涡和南亚高压的活动与东北区夏季低温的关系. 气象学报, (4): 483-494. DOI: 10.11676/qxxb1981.052
1981: THE SUMMER ANOMALY LOW TEMPERATURE OF CHINESE NORTHEAST REGION IN CONNECTION WITH THE ACTIVITY OF 100 MB LEVEL POLAR VORTEX AND SOUTHASIA HIGH PRESSURE. Acta Meteorologica Sinica, (4): 483-494. DOI: 10.11676/qxxb1981.052
Citation: 1981: THE SUMMER ANOMALY LOW TEMPERATURE OF CHINESE NORTHEAST REGION IN CONNECTION WITH THE ACTIVITY OF 100 MB LEVEL POLAR VORTEX AND SOUTHASIA HIGH PRESSURE. Acta Meteorologica Sinica, (4): 483-494. DOI: 10.11676/qxxb1981.052

100毫巴极涡和南亚高压的活动与东北区夏季低温的关系

THE SUMMER ANOMALY LOW TEMPERATURE OF CHINESE NORTHEAST REGION IN CONNECTION WITH THE ACTIVITY OF 100 MB LEVEL POLAR VORTEX AND SOUTHASIA HIGH PRESSURE

  • 摘要: 本文利用10O毫巴面资料,计算了位势距平场及纬向地转风速,讨论了极涡、南亚高压的活动与我国东北区夏季低温的关系,得出如下结论:1.中国东北区夏季异常低温的形成,是南亚高压弱、极地冷空气经常在中纬度活动的结果;2.冬季(11—2月)100毫巴太平洋副热带高压与夏季的南亚高压有关系,他们的相关系数等于0.62;3.1—5月100毫巴面极涡的频数分布有三种类型:a.当极涡经常在极区活动时,则东北区夏季气温偏暖;b.当极涡持续偏心在欧亚大陆活动时,则东北区夏季气温偏冷;c.如果极涡的频数分布有两个高频数中心分别在欧亚及北美,则东北区夏季气温的偏暖或偏冷决定于南亚高压的偏高或偏低,他们彼此成正相关;4.东北区夏季气温与欧亚大陆冬季的雪盖面积和青藏高原的降雪量成反相关。

     

    Abstract: In this Paper, we had computed the geopotential anomaly field and the latitude geostrophic wind velocity of north hemispher 100 mb level. It was discussed that the activity of polar vortex and southasia high has a connection with the summer low temperature of Chinese Northeast Region.Following conclusions were obtained: 1.The anomaly cold summer of Chinese Northeast Region is becomed by the weak suthasia high and the usual activity of polar cold air in middle latitude. 2.Winter (Nov-Feb.)100 cob level pacific high has a connection with sucomer southasia high.The correlation coefficient of them is 0.62. 3.It is show that there are three kinds of frequency graphs of five months (Jan.-May.)100 cob level polar vortex: a) When the arctic vortex is always activity in the north polar region, the summer temperature of Chinese Northeast Region is warm. b) When the arctic vortex is always activity in Eurasia, the sucomer temperature of Chinese Northeast Region is cold irrespective of intensity or weak the southasia high. c) When there are two frequency centres of frequency graph of five months (Jan.-May.)arctic vortex located specifically at Eurasia and north America, the summer temperature of Chinese Northeast Region is determined by high or low of southasia high. They are correlation to each other.4.The summer temperature of northeast region has a connection with winter snow-cover Eurasia area and sonwfall of Chinghai-Tibet plateau. They are anti-correlations each other.

     

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