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      Forcing and biological impact of onset of the 1992 El Niño in central California

      Geophysical Research Letters
      American Geophysical Union (AGU)

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          TOGA COARE: The Coupled Ocean—Atmosphere Response Experiment

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            Meteorological aspects of the el nino/southern oscillation.

            The single most prominent signal in year-to-year climate variability is the Southern Oscillation, which is associated with fluctuations in atmospheric pressure at sea level in the tropics, monsoon rainfall, and wintertime circulation over North America and other parts of the extratropics. Although meteorologists have known about the Southern Oscillation for more than a half-century, its relation to the oceanic El Niño phenomenon was not recognized until the late 1960's, and a theoretical understanding of these relations has begun to emerge only during the past few years. The past 18 months have been characterized by what is probably the most pronounced and certainly the best-documented El Niño/Southern Oscillation episode of the past century. In this review meteorological aspects of the time history of the 1982-1983 episode are described and compared with a composite based on six previous events between 1950 and 1975, and the impact of these new observations on theoretical interpretations of the event is discussed.
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              Experimental forecasts of El Niño

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                Author and article information

                Journal
                Geophysical Research Letters
                Geophys. Res. Lett.
                American Geophysical Union (AGU)
                00948276
                February 01 1996
                February 01 1996
                : 23
                : 3
                : 265-268
                Article
                10.1029/96GL00017
                21b7786c-5872-4491-a426-6add717338ac
                © 1996

                http://doi.wiley.com/10.1002/tdm_license_1.1

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