拉萨和南京大气层下部的气候变化及其与环境因子的联系  

CLIMATIC CHANGE OF LOWER ATMOSPHERE OVER LHASA,NANJING AND ITS CONNECTION WITH ENVIRONMENTAL FACTORS

作　　者：葛玲[1] 赵远东[1] 梁佳兴 宋连春[2] 

机构地区：[1]南京气象学院大气科学系,南京210044 [2]中国气象局国家气象中心,北京100081

出　　处：《南京气象学院学报》1999年第4期663-670,共8页Journal of Nanjing Institute of Meteorology

基　　金："九五"国家"短期气候预测研究"项目;南京市留学回国人员工作站资助

摘　　要：利用１９５８～１９９５ 年拉萨、南京地区地面至３０ ｈＰａ标准等压面上月平均气温资料，研究了青藏高原主体东部的拉萨地区上空若干气候特征以及月、季、年平均气候变率随高度分布特点，并与同纬带长江三角洲的南京地区作了比较。还讨论了两地区平流层下部 对流层中部气候变化与亚欧高纬地区大气臭氧总量及南亚高压变化的联系。By using the monthly mean temperature data from surface up to 30hPa in 1958~1995 over Lhasa and Nanjing,investigated are several climatic features and vertical distribution characteristic of monthly,seasonal and annual temperature variability over Lhasa with the conditions over Nanjing compared.The relationship is also discused between the climatic change at low stratosphere and middle troposphere over the two stations on one hand,and total ozone at high latitudes over Eurasian continent and the south Asia high on the other hand.

关 键 词：南京市 气候变化 臭氧总量 大气层 环境因子 

分 类 号：P467[天文地球—大气科学及气象学] P421.33