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SlideshowReport

Upwelling Between ENSOs and El Niño Southern Oscillation

Description
(a) Westward flow of cold, surface water between ENSOs. (b) Eastward dislocation of warm water during El Niño.

clear skies, dry descending air masses, high pressure warm, moist, ascending air masses, low pressure, storms in western Pacific upwelling of cold water to 307160 feet below surface A warm, moist, | k' ascending air c ear s Ies, descending air ' 5 0‘" wes\ masses, low _ pressure, masses, high storms pressure */”Téirifalls in central Pacific no upwelling; cold water as deep as 500 feet below surface
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