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A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature

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Bjerknes, J.·1966·Tellus A: Dynamic Meteorology and Oceanography

Abstract

Weakness and temporary elimination of the equatorial easterly winds over the eastern and central Pacific in late 1957 and early 1958 brought about a brief cessation of equatorial upwelling which in turn caused the occurrence of above-normal surface water temperatures in the tropical Pacific from the American coast westward to the dateline. This sudden introduction of a large anomalous heat source for the atmosphere intensified its thermodynamic circulation, especially in the wintertime (northern) hemisphere. Record intensity of the westerlies resulted in the eastern North Pacific. The anomalous depth of the Low in the Gulf of Alaska had the downwind effect of weakening the Iceland Low and setting the stage for a cold winter in northern Europe.

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Metadata

Authors
Bjerknes, J.
Venue
Tellus A: Dynamic Meteorology and Oceanography
Published
1966-01-01
Volume
18
Issue
4
Pages
820
ISSN
  • 0280-6495 (ISSN-L)
  • 1600-0870
OpenAlex
W4256444905
Cited by
509
References
0
FWCI
3.39
Type
journal article
Language
en
Open access
hybrid

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CoChat. (2026). Citation check: A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature. https://app.cochat.ai/papers/10.3402/tellusa.v18i4.9712
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Bjerknes, J. (1966). A possible response of the atmospheric Hadley circulation to equatorial anomalies of ocean temperature. Tellus A: Dynamic Meteorology and Oceanography. https://doi.org/10.3402/tellusa.v18i4.9712

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.