Editorial Type:
Article
Article Type:
Research Article

The 1976/77 North Pacific Climate Regime Shift: The Role of Subtropical Ocean Adjustment and Coupled Ocean–Atmosphere Feedbacks

Lixin Wu Physical Oceanography Laboratory, Ocean University of China, Qingdao, China

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Dong Eun Lee Center For Climatic Research, University of Wisconsin—Madison, Madison, Wisconsin

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Zhengyu Liu Center For Climatic Research, University of Wisconsin—Madison, Madison, Wisconsin

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Print Publication:
01 Dec 2005
DOI:
https://doi.org/10.1175/JCLI3583.1
Page(s):
5125–5140
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Abstract

In this study, a new modeling approach is used to look for potential causes of the North Pacific decadal climate regime shift. This new modeling approach is specifically designed to assess not only how changes of the wind-driven ocean circulation induce SST variability, but also the subsequent feedback to climate. Observations appear to indicate that the 1970s North Pacific climate regime shift may be attributed to the coupled ocean–atmosphere interaction over the North Pacific in response to persistent wind stress anomalies in the previous decade. This tends to be supported by modeling results, which suggest that the delayed adjustment of the subtropical ocean circulation may generate sea surface temperature (SST) anomalies in the western subtropical Pacific that may potentially induce a shift of atmospheric circulation, leading to a change of SST in the central and midlatitude North Pacific. This study appears to unify the recent contradictory views of the roles of ocean circulation in the North Pacific decadal climate variability.

* Center for Climatic Research Contribution Number 866

Corresponding author address: Dr. Lixin Wu, Physical Oceanography Laboratory, College of Physical and Environmental Oceanography, Ocean University of China, 5 Yushan Road, Qingdao 266003, China. Email: lixinwu@wisc.edu

Abstract

In this study, a new modeling approach is used to look for potential causes of the North Pacific decadal climate regime shift. This new modeling approach is specifically designed to assess not only how changes of the wind-driven ocean circulation induce SST variability, but also the subsequent feedback to climate. Observations appear to indicate that the 1970s North Pacific climate regime shift may be attributed to the coupled ocean–atmosphere interaction over the North Pacific in response to persistent wind stress anomalies in the previous decade. This tends to be supported by modeling results, which suggest that the delayed adjustment of the subtropical ocean circulation may generate sea surface temperature (SST) anomalies in the western subtropical Pacific that may potentially induce a shift of atmospheric circulation, leading to a change of SST in the central and midlatitude North Pacific. This study appears to unify the recent contradictory views of the roles of ocean circulation in the North Pacific decadal climate variability.

* Center for Climatic Research Contribution Number 866

Corresponding author address: Dr. Lixin Wu, Physical Oceanography Laboratory, College of Physical and Environmental Oceanography, Ocean University of China, 5 Yushan Road, Qingdao 266003, China. Email: lixinwu@wisc.edu

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