江苏冬夏极端气温与大气环流及海温场的遥相关

何卷雄; 丁裕国; 姜爱军

江苏冬夏极端气温与大气环流及海温场的遥相关

1.
南京气象学院江苏南京 210044
2.
江苏省气象局江苏南京 210093

基金项目: 江苏省自然科学基金项目(BK97183)资助

计量
- 文章访问数: 948
- HTML全文浏览量: 0
- PDF下载量: 782
- 被引次数: 0
出版历程
- 收稿日期: 2000-10-12
- 修回日期: 2001-03-26

TELECONNECTION BETWEEN SUMMER AND WINTER EXTREMETEMPERATURE OF JIANGSU, SST AND 500 HPA FIELD

1.
Nanjing Institute of Meteorology, Nanjing 210044, China
2.
Jiangsu Meteorological Bureau, Nanjing 210093, China

摘要

摘要: 以江苏夏季最高气温和冬季最低气温场为例,研究海气耦合作用对区域气温场异常型态的影响。结果表明,江苏夏季最高气温受到同期海气耦合作用的影响较明显,冬季最低气温受同期海气耦合作用的影响较少;从一定意义上说,夏季最高气温的降低是由于东太平洋遥相关型强度的变化及同期北太平洋海温距平分布型的强度加强所致,而冬季最低气温的升高则是由于WA型及欧亚大陆上空环流型强度的变化及同期北太平洋海温距平分布型的强度减弱所致。
- 夏季最高气温 /
- 冬季最低气温 /
- 遥相关
Abstract: We made a study on relationship between summer maximum and winter minimum temperature of Jiangsu, SST and 500 hPa field in order to understand how air-ocean interaction influences on regional climatic anomalous pattern. Summer air-ocean interaction makes a strong impact on summer maximum temperature in Jiangsu. Winter air-ocean interaction has a little influence on winter minimum temperature. The strengthening of eastern Pacific pattern (EP) and the change of distribution of summer northern Pacific SST anomaly account for the drop of summer maximum temperature. The weakening of the distribution of summer northern Pacific SST anomaly and the variation of WA pattern and Eurasia circulation account for the rise of winter minimum temperature.
- summer maximum temperature /
- winter minimum temperature /
- teleconnection

HTML全文

参考文献(15)

[1]	DEGAETANO A T. Recent trends in maximum and minimum temperature threshold in the northern United States[J].J C, 1996, 9(7):1646-1660.
[2]	屠其璞, 丁裕国, 侯淑梅. 我国平均气温升高时极端气温的变化[A]. 气候学研究(第4辑)[C]. 北京:气象出版社, 1996.128-134.
[3]	丁一汇. 高等天气学[M]. 北京:气象出版社, 1991. 745-766.
[4]	余志豪, 蒋全荣. 厄尔尼诺,反厄尔尼诺和南方涛动[M]. 南京:南京大学出版社, 1994. 262-325.
[5]	陈烈庭. 太平洋海气相互作用时空变化[J]. 气象学报, 1983, 41: 296-304.
[6]	HOREL J D, WALLACE J M. Planetary-Scale atmospheric phenomena associated with the southern oscillation[J]. MonWea Rev, 1981,109(4):813-829.
[7]	魏凤英, 张先恭. 北太平洋海表温度与中国夏季气温的耦合特征[A]. 我国短期气候变化及成因研究[C]. 北京:气象出版社, 1996. 67-74.
[8]	WALLACE J M, GUTZLER D S. Teleconnections in the geopotential height field during the northern hemisphere winter[J].Mon Wea Rev, 1981, 109: 813-829.
[9]	吴国雄, 王敬芳. 冬季中高纬500 hPa高度和SST异常特征及其相关分析[J]. 气象学报, 1997, 55: 11-21.
[10]	WALLACE J M, SMITH C,. BRETHERTON C S. SVD of wintertime sea surface temperature and 500 mb heightanomalies[J]. J Climate, 1992, 5: 567-576.
[11]	NITTA T. Convective activities in the tropical western Pacific and their impact on the northern hemisphere summercirculation[J]. J Meteor Soc Japan,1987, 65: 373-390.
[12]	施能. 北半球冬季大气环流遥相关型的长期变化及其与我国气候变化[J]. 气象学报, 1996, 54: 673-683.
[13]	黄荣辉. ENSO及热带海气相互作用动力学研究的新进展[J]. 大气科学, 1990, 14: 234-242.
[14]	丁裕国, 江志红. SVD方法在气象诊断分析中的普适性[J]. 气象学报, 1996, 54: 365-372.
[15]	姜爱军, 董晓敏. 江苏省近40年温度变化的诊断分析[J]. 气象, 1991(1): 34-38.