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青藏高原臭氧的准两年振荡
引用本文:季崇萍,邹捍,周立波.青藏高原臭氧的准两年振荡[J].气候与环境研究,2001,6(4):416-424.
作者姓名:季崇萍  邹捍  周立波
作者单位:中国科学院大气物理研究所环境与极地研究部,北京,100029
基金项目:国家自然科学基金资助项目49775276、中国科学院大气物理研究所重点知识创新项目8-2212和中国科学院重大项目KZ951-A-205-05
摘    要:通过对臭氧卫星观测资料及大气环流资料的分析,研究了青藏高原上空臭氧的季节和年际变化.通过分析青藏高原地区臭氧准两年振荡(QBO),并与同纬度无山区及赤道地区臭氧QBO进行比较,指出:青藏高原臭氧QBO的平均周期为29个月,平均振幅为8DU.青藏高原臭氧QBO变化位相与热带平流层纬向风场QBO相反,即热带平流层纬向西风时,青藏高原上空臭氧总量偏小,东风时臭氧总量偏大.还讨论了与青藏高原臭氧QBO相关的大气环流物质输送理论.

关 键 词:臭氧  准两年振荡  年际变化  物质输送
修稿时间:2000年1月6日

QBO Signal in Total Ozone Over the Tibet
Ji Chongping,Zou Han and Zhou Libo.QBO Signal in Total Ozone Over the Tibet[J].Climatic and Environmental Research,2001,6(4):416-424.
Authors:Ji Chongping  Zou Han and Zhou Libo
Abstract:From data analysis of ozone satellite observation and general circulation, this article dis-cusses the seasonal and inter-annual variations of total ozone over the Tibet. Analysis has been done on quasi-biennial oscillation (QBO) in inter-annual ozone variation over the Tibet, in comparison with QBO over the tropics and non-mountain region at the same latitudes of the Tibet. The fact is shown that the Tibet ozone QBO has averaged period 29 months, with averaged amplitude S DU. The Tibet ozone QBO is anti-phase against the stratospheric wind QBO over the tropics, i.e., when the tropics 30 hPa-wind is easterly, ozone has a surplus, and vice verse. This article also discusses the impact of atmospheric transfer on ozone QBO over the Tibet.
Keywords:ozone  quasi-biennial oscillation  inter-annual variation  mass transportation  
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