%0 Journal Article
%T Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle<br>TBO的原因－异常东亚冬季风与ENSO循环的相互作用
%A Li Chongyin
%A Sun Shuqing
%A Mu Mingquan
%A <br>Li Chongyin
%A Sun Shuqing
%A Mu Mingquan
%J 大气科学进展
%D 2001
%I 
%X Based on the data analyses by using NCEP/NCAR reanalysis data and other data (OLR, precipitation and temperature), it is shown that the tropospheric circulation and climate in East Asia and the northwestern Pacific region have the evident quasi-biennial oscillation (TBO) feature. It is also shown that anomalous East Asian winter monsoon can impact the atmospheric circulation and climate variations in the following summer, particularly in East Asian region; there is clear interaction between anomalous East Asian winter monsoon and ENSO cycle. The continuous strong (weak) East Asian winter monsoon can excite El Nino (La Nina) through the air-sea interaction, the El Nino (La Nina) event can lead the East Asian winter monsoon to be weak (strong) through the teleconnections or remote responses. The strong or weak winter monsoon and ENSO cycle are linked each other. It can be suggested that interaction between anomalous East Asian winter monsoon and ENSO cycle is a fundamental origin of the TBO.
%K Origin
%K Tropospheric biennial oscillation (TBO)
%K Interaction
%K Anomalous East Asian winter monsoon
%K ENSO cycle<br>原因
%K 对流层准两年振荡(TBO)
%K 相互作用
%K 异常东亚冬季风
%K ENSO循环
%U http://www.alljournals.cn/get_abstract_url.aspx?pcid=E62459D214FD64A3C8082E4ED1ABABED5711027BBBDDD35B&cid=28A2F569B2458C17&jid=5434AFBF6CB6E7E8D67733B541F211C7&aid=4F9A7FC40187A5A78B0FA4802CD8F55A&yid=14E7EF987E4155E6&vid=13553B2D12F347E8&iid=E158A972A605785F&sid=D8414BC1307BF1A3&eid=CDC418F38C4BFD60&journal_id=0256-1530&journal_name=大气科学进展&referenced_num=18&reference_num=29