Tropical Ocean-Atmosphere Interaction, the Pacific Cold Tongue, and the El Niño-Southern Oscillation

1996 Science 214 citations

Abstract

The tropical Pacific basin allows strong feedbacks among the trade winds, equatorial zonal sea surface temperature contrast, and upper ocean heat content. Coupled atmosphere-ocean dynamics produce both the strong Pacific cold tongue climate state and the El Niño-Southern Oscillation phenomenon. A simple paradigm of the tropical climate system is presented, capturing the basic physics of these two important aspects of the tropic Pacific and basic features of the climate states of the Atlantic and Indian ocean basins.

Keywords

ClimatologyAtmosphere (unit)Sea surface temperatureOcean heat contentPacific decadal oscillationOceanographyStructural basinOceanic basinEl Niño Southern OscillationGeologyTropical climateSouthern oscillationPacific oceanEnvironmental scienceGeographyMeteorologyPaleontology

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Publication Info

Year
1996
Type
article
Volume
274
Issue
5284
Pages
76-78
Citations
214
Access
Closed

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Fei‐Fei Jin (1996). Tropical Ocean-Atmosphere Interaction, the Pacific Cold Tongue, and the El Niño-Southern Oscillation. Science , 274 (5284) , 76-78. https://doi.org/10.1126/science.274.5284.76

Identifiers

DOI
10.1126/science.274.5284.76