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大气季节内振荡研究进展
引用本文:杨双艳,武炳义,周顺武,刘炜. 大气季节内振荡研究进展[J]. 气象科技, 2012, 40(6): 938-948
作者姓名:杨双艳  武炳义  周顺武  刘炜
作者单位:1. 中国气象科学研究院,北京100081;南京信息工程大学,气象灾害省部共建教育部重点实验室,南京210044
2. 中国气象科学研究院,北京,100081
3. 南京信息工程大学,气象灾害省部共建教育部重点实验室,南京210044
基金项目:国家自然科学基金项目,公益性行业(气象)科研专项,中国气象科学研究院基本科研业务经费
摘    要:大气季节内振荡(ISO:Intra-Seasonal Oscillation)主要是指时间尺度为30~60天的振荡,它是大气中最显著的一种振荡现象.作为大气的一个重要低频系统,自20世纪70年代至今的近40年中,ISO已经受到了广泛的关注,且已取得众多有意义的研究成果.ISO对调整气候变率起重要作用,对我国天气气候有着深远的影响.该文较系统地总结了近年来ISO的研究成果,主要对它的结构和活动特征、对天气气候的影响及其激发维持机制等方面进行了综述.在此基础上,对今后的一些研究重点进行了展望.

关 键 词:季节内振荡  低频系统  活动特征  气候变率
收稿时间:2011-07-23
修稿时间:2011-11-11

Progress in Researches on Atmospheric Intraseasonal Oscillation
Yang Shuangyan,Wu Bingyi,Zhou Shunwu and Liu Wei. Progress in Researches on Atmospheric Intraseasonal Oscillation[J]. Meteorological Science and Technology, 2012, 40(6): 938-948
Authors:Yang Shuangyan  Wu Bingyi  Zhou Shunwu  Liu Wei
Affiliation:1 Chinese Academy of Meteorological Sciences, Beijing 100081; 2 Key Laboratory of Meteorological Disaster of Ministry of Education, NUIST, Nanjing 210044;Chinese Academy of Meteorological Sciences, Beijing 100081;Key Laboratory of Meteorological Disaster of Ministry of Education, NUIST, Nanjing 210044;Key Laboratory of Meteorological Disaster of Ministry of Education, NUIST, Nanjing 210044
Abstract:The intra srasonal oscillation of the atmosphere (ISO) mainly indicates the oscillation at a time scale of 30 to 60 days, one of the most remarkable oscillation phenomenans. As one of the most distinct low frequency systems, ISO has been paid great attention widely, and already obtained numerous meaningful results since the 1970s. ISO plays a crucial role in adjusting climate variability and influences weather and climate of China profoundly. A systemic summary is made of the researches on ISO in the recent years, with emphases on its structure, activity characteristics, influence on weather and climate, stimulation, and maintaining mechanisms. The prospects of further studies about ISO are discussed based on those summaries.
Keywords:intra srasonal oscillation   low frequency system   activity characteristic   climate variability
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