On the equatorial Pacific response to the 1982/1983 EI Nino—Southern Oscillation event

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ID: 298785
1984
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Abstract
The ocean's response to the 1982/83 El Nino-Southern Oscillation event was the largest ever documented. In this paper the authors explore the effects of certain details of the observed zonal wind stress anomaly field upon the ocean's response using a linear, adiabatic, reduced gravity, analytical model. The increase in magnitude of the downwelling response over the composite of previous El Nino events is attributed to the eastward translation of the observed westerly wind anomaly and the double peaked downwelling at the South American coast is attributed to the amplitude modulation of this anomaly. Effects of an easterly anomaly which appeared to the west of the dateline midway through the event are also considered.
Reference Key
openalex_W192750932 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors T. Y. Tang, Robert H. Weisberg
Journal journal of marine research
Year 1984
DOI
10.1357/002224084788520765
URL
https://doi.org/10.1357/002224084788520765
Keywords Keywords not found

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