NDLI: Origin of the Tbo-Interaction between anomalous east-Asian winter monsoon and enso cycle

Content Provider	Springer Nature Link
Author	Chongyin, Li Shuqing, Sun Mingquan, Mu
Copyright Year	2001
Abstract	Based on the data analyses by using NCEP/ NCAR reanalysis data and other data (OLR, precipita-tion 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 ex-cite El Niño (La Niña) through the air-sea interaction, the El Niño (La Niña) 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 anoma-lous East Asian winter monsoon and ENSO cycle is a fundamental origin of the TBO.
Starting Page	554
Ending Page	566
Page Count	13
File Format	PDF
ISSN	02561530
Journal	Advances in Atmospheric Sciences
Volume Number	18
Issue Number	4
e-ISSN	18619533
Language	English
Publisher	Science Press
Publisher Date	2001-01-01
Publisher Place	Beijing
Access Restriction	One Nation One Subscription (ONOS)
Subject Keyword	Origin Tropospheric biennial oscillation (TBO) Interaction Anomalous East Asian winter monsoon ENSO cycle Meteorology/Climatology Geophysics/Geodesy
Content Type	Text
Resource Type	Article
Subject	Atmospheric Science

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