###
气象:2013,39(9):1096-1102
本文二维码信息
码上扫一扫!
冬季欧亚型遥相关候时间尺度异常特征及其对我国天气的影响
(1.河南省气候中心,郑州 450003,南京信息工程大学,大气科学学院,南京 210044;2.中国气象局气象干部培训学院,北京 100081,中国科学院大气物理研究所,北京 100029)
Abnormal Characteristics of Eurasian Teleconnection in Winter at Pentad Time Scale and Its Impact on the Weather in China
(1.Henan Climate Centre, Zhengzhou 450003,Department of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044;2.China Meteorological Administration Training Centre, Beijing 100081,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029)
摘要
图/表
参考文献
相似文献
本文已被:浏览 1082次   下载 3159
投稿时间:2012-11-17    修订日期:2013-05-13
中文摘要: 本文利用NCEP/NCAR全球逐日再分析资料,确定了冬季欧亚(EU)型遥相关逐候指数持续性异常的标准,继而分析了EU指数持续性异常的特征,探讨了对应时段的环流特征及其对我国冬季天气的影响。统计结果表明:1957—2010年的54个冬季共发生了26次异常过程;正、负异常过程各有三个高发时段分别为12月、1月第2—5候、2月第4候至3月第1候,以及12月第4—5候、1月前3候、2月第3候至3月第1候。选取200、850 hPa分别代表高低层大气,对异常过程合成分析后发现:指数异常时,高低层大气具有强的EU型特征;我国大部分地区的气温受EU指数异常影响,差异显著;黄河中下游、长江中下游及东南局部地区的降水差异显著;正异常过程中,受西伯利亚高压加强的影响,我国对流层低层盛行偏北风,温度普遍偏低,降水偏少;负异常过程相反。
Abstract:Using the NCEP/NCAR global daily reanalysis data, this paper defined the winter pentad Eurasian teleconnection persistent anomaly, analyzed the characteristics of persistent abnormal process of EU pattern and discussed the corresponding atmospheric circulation and its impact on the winter weather in China. Statistical results show that: 26 persistent abnormal processes occur in the 54 winters of 1957-2010. The positive persistent abnormal processes mainly occur in December, the 2nd to the 5th pentad of January, and the 4th pentad of February to the 1st pentad of March while the negative ones occur in the 4th and 5th pentads of December, the first three pentads of January and the 3rd pentad of February to the 1st pentad of March. Then the 200 hPa and 850 hPa geopotential height fields are selected to represent high and low atmospheric layers. Synthetic analysis shows that: during the processes of index anomalies, characteristics of strong EU pattern exists in both of the high and low atmospheric layers; and temperature in most parts of China is influenced by EU index anomalies, showing significant difference. Precipitation presents significant difference in the middle and lower reaches of the Yellow River and Yangtze River, and parts of southeastern China. During positive abnormal processes, influenced by the strengthened Siberian high, northerly winds prevail in the lower troposphere over China with lower temperature and less rainfalls. The opposite situation tends to occur in negative processes.
文章编号:     中图分类号:    文献标志码:
基金项目:公益性行业(气象)科研专项(GYHY201106015)资助
引用文本:
左璇,肖子牛,2013.冬季欧亚型遥相关候时间尺度异常特征及其对我国天气的影响[J].气象,39(9):1096-1102.
ZUO Xuan,XIAO Ziniu,2013.Abnormal Characteristics of Eurasian Teleconnection in Winter at Pentad Time Scale and Its Impact on the Weather in China[J].Meteor Mon,39(9):1096-1102.