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La Nina

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La Niña  (lä nnyä)
A cooling of the surface water of the eastern and central Pacific Ocean, occurring somewhat less frequently than El Niño events but causing similar, generally opposite disruptions to global weather patterns. La Niña conditions occur when the Pacific trade winds blow more strongly than usual, pushing the sun-warmed surface water farther west and increasing the upwelling of cold water in the eastern regions. Together with the atmospheric effects of the related southern oscillation, the cooler water brings drought to western South America and heavy rains to eastern Australia and Indonesia. Compare El Nino.


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As many previous studies had noted, the number and strength of tropical cyclones were markedly lower in El Nino years than during La Nina episodes, when sea-surface temperatures in the eastern and central Pacific are substantially cooler than normal.
Published in the journal Weather, Manoj Joshi suggests that the Australian Cricket team is more likely to succeed after El Nino years when the series is held in Australia, while the England cricket team has a historically better record following La Nina years, the opposite phase.
La Nina is produced by cooler surface water temperatures in the Pacific Ocean and, like its Pacific sibling El Nino, is credited with upsetting climate patterns around the world.
 
 
 
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