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Cited by 170

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A pan‐Atlantic decadal climate oscillation

Xie, Shang‐Ping, Tanimoto, Youichi·1998·Geophysical Research Letters

Abstract

Sea surface temperature (SST) variabilities on time scales of 10–14 years have been documented in various parts of the Atlantic Ocean. Here we present observational evidence that these regional variabilities are part of a coherent pan‐Atlantic decadal oscillation (PADO) characterized by zonal bands of SST and wind anomalies stacked in the meridional direction with alternate polarities from the South Atlantic all the way to Greenland. We propose that the interaction of wind, evaporation and SST is key to establishing this interhemispherical PADO, based on results from a new ocean‐atmosphere coupling model. Forced by extratropical wind forcing, the model successfully reproduces the observed decadal oscillation in both SST and wind velocity over the Tropics. This decadal extratropical forcing of the Tropics is in sharp contrast to the well‐known Tropics‐to‐extratropics teleconnection that operates on interannual time scales in association with El Nino/Southern Oscillation (ENSO).

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Metadata

Authors
Xie, S., & Tanimoto, Y.
Venue
Geophysical Research Letters
Published
1998-06-15
Volume
25
Issue
12
Pages
2185-2188
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2027769450
Cited by
170
References
1
FWCI
12.07
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: A pan‐Atlantic decadal climate oscillation. https://app.cochat.ai/papers/10.1029/98gl01525
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Xie, S., & Tanimoto, Y. (1998). A pan‐Atlantic decadal climate oscillation. Geophysical Research Letters. https://doi.org/10.1029/98gl01525

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