Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation

Zhao Yongping; G. A. McBean

doi:10.1007/BF02842748

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Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation

Updated：2023-05-16

- Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation
- Journal of Oceanology and Limnology Vol. 7, Issue 2, Pages: 123-134(1989)
- Affiliations：
  
  1. Institute of oceanology
  2. Canadian Climate Centre
- Author bio：
- Funds：
- DOI：10.1007/BF02842748
  CLC：
- Published：1989
- Accepted：
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Yongping, Z., McBean, G.A. Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation., Chin. J. Ocean. Limnol. 7, 123–134 (1989). https://doi.org/10.1007/BF02842748
DOI：

Yongping, Z., McBean, G.A. Principal North Pacific heating anomaly patterns and their relations to the atmospheric circulation., Chin. J. Ocean. Limnol. 7, 123–134 (1989). https://doi.org/10.1007/BF02842748 DOI：

摘要

Abstract

The principal variability patterns (EOF) of the anomalies of total heat transfer from ocean to atmosphere computed from 30 years' monthly averaged data over the North Pacific Ocean (20°–60°N) showed variability was dominated by two patterns: a bipolar pattern and a dominantly positive or negative pattern depending on the sign of the time series coefficients. The atmosphere contributes greatly to the marine heating anomalies in most of the North Pacific in all seasons. In winter

a positive feedback is formed between the Aleutian Low and the marine heating anomalies; in summer

the marine heating anomalies are controlled by the heating on the Qinghai-Tibetan Plateau. Both patterns have a winter correlation with the Southern Oscillation Index.

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references

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