Cited by 42Climate variability and modelsOceanographic and Atmospheric ProcessesMeteorological Phenomena and Simulations

How and why climate variability differs between the tropical Atlantic and Pacific

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Xie, Shang‐Ping, Tanimoto, Youichi, Noguchi, Hideyuki, Matsuno, Taroh·1999·Geophysical Research Letters

Abstract

The tropical Pacific and Atlantic Oceans share many common climatological features such as easterly trade winds, eastward shoaling thermocline, an eastern cold tongue and a northerly intertropical convergence zone (ITCZ). However, a comparison of climate variability between the two oceans reveals more differences than similarities. The Pacific is dominated by the equatorially symmetric El Nino/Southern Oscillation (ENSO) while the Atlantic ITCZ is controlled by changes in interhemispheric sea surface temperature (SST) gradient. To understand the causes of these differences in variability, a dynamic ocean‐atmosphere coupling model is developed that includes both the Bjerknes and wind‐evaporation‐SST feedbacks. Equatorially symmetric and anti‐symmetric modes emerge from the model, displaying distinct growth rate dependence on zonal wavenumber. Consistent with observations, an equatorially trapped ENSO mode dominates an ocean with a longitudinal size of the Pacific while in a smaller Atlantic‐size one, a monopole mode with a broad meridional scale coexists with an equatorially anti‐symmetric dipole mode.

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Crossref · 10.1029/1999gl900308

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  • Two primary modes of interannual variability have been identified in the tropical Atlantic: the equatorial and meridional modes.

    “Within the last decades, two primary modes of interannual variability have been identified in the tropical Atlantic (e.g.Servain andMerle, 1993, Xie et al., 1999)): the equatorial and meridional modes.”

    From Sea surface temperature patterns in the Tropical Atlantic: Principal component analysis and nonlinear principal component analysis (2017) · cites this paper as Xie et al., 1999

    The Observational Background (page unavailable in our copy) favors two tropical Atlantic modes: an equatorially symmetric monopole and an antisymmetric dipole. But it describes the monopole as interannual and the dipole as decadal, so it does not support calling both modes interannual. (LLM, conf=0.88)

    Experimental — accuracy not yet measured

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  1. Y. Tanimoto, T. Matsuno, Frontier Research System for Global Change, 1-2-1 Shibaura, Minato, Tokyo 105-6791, Japan (e-mail: tan i mot o @ fro n tier. esto. or.j p ) (Received February 18, 1999; revised April 7, 1999; accepted April 13, 1999) 19448007, 1999, 11, Downloaded from https://agupubs.onlinelibrary.wiley.com/doi/10.1029/1999GL900308 by Readcube (Labtiva Inc.), Wiley Online Library on [16/08/2023]. See the Terms and Conditions (https://onlinelibrary.wiley.com/terms-and-conditions) on Wiley Online Library for rules of use; OA articles are governed by the applicable Creative Commons License · DOI

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Authors
Xie, S., Tanimoto, Y., Noguchi, H., & Matsuno, T.
Affiliations
Hokkaido University (JP)
Venue
Geophysical Research Letters
Published
1999-06
Volume
26
Issue
11
Pages
1609-1612
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2006068451
Cited by
42
References
1
Citations by year
2026: 1 · 2025: 1 · 2023: 1 · 2022: 1 · 2021: 1 · 2020: 2 · 2019: 2 · 2017: 2 · 2016: 1 · 2014: 1 · 2013: 1 · 2012: 3
FWCI
4.73
Type
journal article
Language
en
Open access
Locations
Geophysical Research Letters (publishedVersion)
Topics
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Meteorological Phenomena and Simulations
Keywords
tropical Pacific variability, ENSO, Intertropical Convergence Zone, Bjerknes feedback, wind-evaporation-SST feedback, ocean-atmosphere interaction, monopole mode, dipole mode

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