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The ocean surface pressure is lower in the West Pacific compared to Central Pacific and East Pacific and hence Trade winds blow Westwards from the East Pacific towards the West Pacific. The ocean current also moves from East to West. Upwelling of cold water takes place near the coast of Peru\/Equador. These deeper waters have nutrients that stimulate the growth of microscopic photosynthetic algae (“Phytoplankton<\/span>“). Phytoplankton, in turn, serve as food for the zooplankton<\/span>. Both phytoplankton and zooplankton serve as food for fish<\/span>\u00a0thereby increasing the fish production in the East Pacific. <\/p>\n El Nino is\u00a0a weather phenomenon that occurs in the Equatorial Pacific Ocean normally of 6 to 18 months time frame\u00a0when there is an abnormal warming of surface ocean waters in the Eastern & Central Equatorial Pacific Ocean. This occurs when the normal trade winds weaken (or even reverse), which lets the warm water that is usually found in the western Pacific to flow instead towards the east. This warm water displaces the cooler water that is normally found near the surface of the eastern Pacific, setting off atmospheric changes that affect weather patterns in many parts of the world.\u00a0Upwelling deep water near the coast of Peru\/Equador is now warm and\u00a0do not have nutrients that stimulate the growth of microscopic photosynthetic algae (“P<\/span>hytoplankton“) and the zooplankton<\/span>. This in turn<\/span>\u00a0decreases the fish production in the East Pacific. This is why these conditions are called El Ni\u00f1o which is Spanish for “the boy”, and the term El Ni\u00f1o refers to the Christ child, Jesus, because this periodic abnormal weather pattern is usually noticed around Christmas.<\/p>\n What happens to the ocean also affects the atmosphere. Tropical thunderstorms are fueled by hot, humid air over the oceans. The hotter the air, the stronger and bigger the thunderstorms. As the Pacific’s warmest water spreads eastward, the biggest thunderstorms move with it. Thus, rains which normally would fall over the tropical rain forests of Indonesia start falling over the central & east Pacific ocean along with deserts of Peru.<\/p>\n <\/p>\n <\/p>\n The Southern Oscillation is the see-saw pattern of reversing surface air pressure between the eastern and western tropical Pacific; when the surface pressure is high in the eastern tropical Pacific it is low in the western tropical Pacific, and vice-versa. Because the ocean warming and pressure reversals are, for the most part, simultaneous, scientists call this phenomenon the El Nino\/Southern Oscillation or ENSO for short.<\/p>\n During an El Nino higher than average air pressure covers Indonesia and the western tropical Pacific and below-average air pressure covers the eastern tropical Pacific. These pressure departures are reversed during La Nina, which features below-average air pressure over Indonesia and the western tropical Pacific and above-average air pressure over the eastern tropical Pacific.<\/span><\/p>\n The Southern Oscillation Index (SOI) is designed to measure the strength and phase of the Southern Oscillation. The SOI is calculated using departures from normal in the surface air pressure difference between Tahiti, French Polynesia and Darwin, Australia.<\/p>\n During El Nino episodes the SOI has a large negative value due to lower-than-average air pressure at Tahiti and higher-than-average pressure at Darwin.<\/span><\/p>\n During La Nina episodes the SOI has a positive value due to higher-than-average air pressure at Tahiti and lower-than-average pressure at Darwin.<\/p>\n","protected":false},"excerpt":{"rendered":" El Nino El Nino is a weather phenomenon that occurs in the Equatorial Pacific Ocean normally lasting between 6 to 18 months. \u00a0First we should understand the normal conditions in the Equatorial Pacific Ocean to better understand about an El Read More …<\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-6011","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=\/wp\/v2\/pages\/6011","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=6011"}],"version-history":[{"count":0,"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=\/wp\/v2\/pages\/6011\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.gujaratweather.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=6011"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
\nDue to high ocean surface temperature in the West Pacific, there is evaporation and clouding and rain over West Pacific while the East Pacific there is dry condition. \u00a0Sun heated warm water piles up in the West Pacific ocean and this is the reason why the temperature of the West Pacific ocean is higher than that of the East Pacific ocean.<\/p>\n<\/a><\/p>\n<\/a><\/p>\n<\/h4>\n
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\nLa Nina is essentially the strengthening of the Normal conditions. During a La Nina, the trade winds strengthens further compared to Normal conditions, which causes the thermocline to tilt further, causing warm water to pool against Australia. The rain follows the location of the warm water, so Australia experiences above average rainfall, while South America experiences below average rainfall.<\/p>\n<\/h4>\n
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El Nino:<\/h4>\n
<\/a><\/p>\n<\/a><\/p>\nSouthern Oscillation ( SOI )<\/span><\/h4>\n