J4 ›› 2008, Vol. 26 ›› Issue (3): 29-33.

• 论文 • 上一篇    下一篇

青藏高原春夏季温度与太平洋海温的关系

刘青春,时兴合,汪青春,冯蜀青,赵永业   

  1. 青海省气象局,青海 西宁 810001)
  • 收稿日期:2008-01-02 修回日期:2008-06-16 出版日期:2008-09-30 发布日期:2008-09-30
  • 作者简介:刘青春(1971 - ) ,女,工程师,主要从事气候变化及青藏高原天气气候研究工作. E-mail: liuqingchunlqc@126. com.
  • 基金资助:

    国家自然科学基金项目“全球气候变化对三江源地区水资源的影响研究(40465002) ”和国家自然科学基金委重大项目“青海湖地区的气候- 构造历史与青藏高原隆升生长及全球变化的联系(40599424) ”共同资助

Rela tion sh ip Between Pac if ic SST and Spr ing, Summer Tempera ture over Qingha i - Xizang Pla teau

L IU Qingchun, SH I Xinghe, WANG Qingchun, FENG Shuqing, ZHAO Yongye   

  1. Q inghai ProvincialM eteorological B ureau, X i’ning 810001, China
  • Received:2008-01-02 Revised:2008-06-16 Online:2008-09-30 Published:2008-09-30

摘要:

从预测高原不同区域春、夏季温度趋势分布的需要出发,利用聚类分析法将高原温度场分为3个区域。通过对3个区春、夏季温度指数与前期太平洋海温相关普查,定义了与高原春、夏季温度指数相关关系清晰的海温分布型指数。冬季西太平洋海温偏高(偏低)的海温分布型造成后期高原II区春季温度偏高(偏低) ;冬季西太平洋海温、东太平洋海温同时偏高(偏低)的海温分布型造成后期高原II区南部、III区夏季温度偏高(偏低) 。进一步分析这2种海温分布型与后期春夏季500 hPa北半球高度场的相关关系,结果表明:当冬季西太平洋海温指数偏高(低)时,春季高度场高纬冷空气活动的势力弱(强)且路径偏北(南) ,同时高原高度场较低(高) ,有利于(不利于)偏南气流北上,有利于(不利于)冬季向夏季环流形势的转变,春季高原中部温度偏高(偏低) ;而当冬季西太平洋、东太平洋海域海温综合指数偏高(低)时,同年夏季500 hPa高度场高原北部至中西伯利亚南部脊加强(减弱) ,高原及北部为高值(低值)系统活动,西太平洋副高偏强(弱) ,夏季高原中部、南部温度偏高(偏低) 。

关键词: 高原春夏季温度, 太平洋海温, 高度场

Abstract:

The clustering analysismethod is used to divide the temperature field in sp ring and summer over the Qinghai - Xizang Plateau into three areas for p redicting the temperature trends of different areas. Based on the correlation between the temperature indexes in sp ring and summer over the Plateau and the Pacific SST in the p receding season, the SST distribution index is defined. When the winter SST over the western Pacific is higher ( lower) than normal, the sp ring temperature in Areas II of the Plateau is higher ( lower) ; while the winter SST in the western and eastern Pacific is higher ( lower) than normal, the summer temperature over southern Areas II and Areas III of the Plateau is higher ( lower) . Further analysis are conducted about the correlation between these two SST distributions and the 500 hPa geopotential height field in sp ring and summer in the Northern Hemisphere. The results show thatwhen the winterwestern Pacific SST index is higher ( lower) , the cold air activities over high latitude weaken ( strengthen) and itsmoving route northward ( southward) ; meanwhile, the geopotential height field is lower ( higher) , it is advantageous ( disadvantageous) to the southern air currentmoving northward and the circulation conversion from the winter type to the summer one, and the sp ring temperature over the central Plateau is higher ( lower) than normal. In contrast, when the integrated index ofwinter SST in the western and eastern Pacific is higher ( lower) , the northern Plateau to southern central - Siberia ridge and the western Pacific subtrop ical high in summer strengthen (weaken) , and the Plateau controlled by high system, the summer temperature over the central and southern Plateau is higher ( lower) .

Key words: sp ring and summer temperature over the Plateau, Pacific SST, geopotential height field

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