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Published byNathan Elliott Modified over 9 years ago
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El Nino and La Nina opposite phases of the El Niño-Southern Oscillation (ENSO) cycle. The ENSO cycle describes the changes in temperature between the ocean and atmosphere in the eastern Pacific Ocean. La Niña is sometimes referred to as the COLD phase of ENSO and El Niño as the WARM phase of ENSO. These changes from normal surface temperatures can have large-scale impacts on ocean processes and on global weather and climate.
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El Nino El Niño refers to periodic warming in sea surface temperatures across the central and east-central Equatorial Pacific. Typical effects of el Nino include warmer-than- average temperatures over western and central Canada, and western and northern United States. Wetter-than-average conditions are likely over the U.S. Gulf Coast and Florida, and drier-than- average conditions in the Ohio Valley and the Pacific Northwest.
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La Nina La Niña episodes represent periods of below-average sea surface temperatures across the east-central Equatorial Pacific. During a La Niña year, winter temperatures are warmer than normal in the Southeast and cooler than normal in the Northwest.
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Hurricane progression
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