Meteorological aspects of El Nino.

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Abstract

Analysis of data from a recently compiled atlas elucidates the role of the annual cycle in modifying the great 1972-73 Nino, and confirms that off S America upwelling and sea surface temperature are not directly linked. Meridional profiles derived from the atlas reveal that oceanic heat loss to the air is a function of wind speed rather than of sea surface temperature and that rainfall can be accounted for in terms of the horizontal convergence of moisture.-from Authors

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APA

Ramage, C. S., & Hori, A. M. (1981). Meteorological aspects of El Nino. Monthly Weather Review, 109(9), 1827–1835. https://doi.org/10.1175/1520-0493(1981)109<1827:MAOEN>2.0.CO;2

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