La Niña

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La Niña:

see El Niño–Southern OscillationEl Niño–Southern Oscillation
(ENSO) , large-scale climatic fluctuation of the tropical Pacific Ocean and the overlying atmosphere. The El Niño [Span.
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References in periodicals archive ?
and Khandekar, M., 1996, The impact of El Nino-Southern Oscillation on the temperature field over Canada: Atmosphere-Ocean, v.
Southern Hemisphere circulation features associated with El Nino-Southern Oscillation events.
Global ecological consequences of the 1982-83 El Nino-Southern Oscillation. Elsevier Oceanography Series 52.
Luis, "Low-frequency changes in El Nino-Southern Oscillation," Journal of Climate, vol.
Scott Power from the Bureau of Meteorology in Melbourne, Australia said that the El Nino-Southern Oscillation cycle more or less reboots around April-May-June each calendar year, New Scientist reported.
Teleconnection between tree growth in the Amazonian floodplains and the El Nino-Southern Oscillation effect.
The El Nino-Southern Oscillation (ENSO) occurrence is a well-known natural element of the global climate system.
At the heart of these changing patterns is a phenomenon called the El Nino-Southern Oscillation (ENSO), a complicated interplay between ocean and atmosphere in the Pacific Ocean.
Outbreak of hantavirus infection in the Four Corners region of the United States in the wake of the 1997-1998 El Nino-Southern Oscillation. J Infect Dis 2000;181:1569-73.
Warmings and coolings in the Pacific represent opposite phases of one basic pattern called the El Nino-Southern Oscillation (ENSO) - a complex duet between ocean currents and wind streams in the tropical Pacific.