Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle

Li Chongyin; Sun Shuqing; Mu Mingquan

doi:10.1007/s00376-001-0044-y

Impact Factor: 5.8

Volume 18 Issue 4

Jul. 2001

Article Contents

Article > ADVANCES IN ATMOSPHERIC SCIENCES > 2001 > 18(4): 554-566

Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle

1.
LASG, Institute of Atmoapheric Physics, Beijing 100029,Institute of Atmospheric Physics, Beijing 100080,LASG, Institute of Atmoapheric Physics, Beijing 100029

doi: 10.1007/s00376-001-0044-y

Abstract
References
Related papers
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Abstract:
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.
- Origin,
- Tropospheric biennial oscillation (TBO),
- Interaction,
- Anomalous East Asian winter monsoon,
- ENSO cycle
References

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Manuscript History

Manuscript received: 10 July 2001

Manuscript revised: 10 July 2001

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Origin of the TBO-Interaction between Anomalous East-Asian Winter Monsoon and ENSO Cycle

1. LASG, Institute of Atmoapheric Physics, Beijing 100029,Institute of Atmospheric Physics, Beijing 100080,LASG, Institute of Atmoapheric Physics, Beijing 100029

Manuscript received: 2001-07-10
Manuscript revised: 2001-07-10

Abstract: 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.

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