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causes and effects of el niño and la niña pdf

Primary Causes of La Niña. Consequently, tropical rains that usually fall over Indonesia shift eastward. In the tropical eastern Pacific during La Niña, strong Trade Winds move water westward, resulting in lower sea level, a rise in the thermocline, and a drop in sea-surface temperature. El Niño conditions occur when abnormally warm waters accumulate in tropical latitudes of the central and eastern Pacific Ocean associated with a weakening of the low-level easterly winds.

El Nino and La Ni˜ na: Causes˜ and Global Consequences Michael J McPhaden National Oceanic and Atmospheric Administration, Seattle, WA, USA El Ni˜no is a warming of the tropical Pacific that occurs roughly every three to seven years and lasts for 12–18 months. In the tropical eastern Pacific during El Niño, weakened Trade Winds results in higher sea level, a deeper thermocline, and warmer sea-surface temperature. It is dynamically linked to the Southern La Niña is caused by the strengthening of the normal steady winds blowing from east to west above and below the equator (trade winds) that usually takes place after an El Niño event.

The effects of El Niño and La Niña and the related shifts in climate risk may be described and explored through analyses of historical impacts and through state-of-the-art numerical climate models. Since during an El Niño the trade winds are weakened, the aftermath is the reinforcement of the winds which reverses the El Niño wind cycle which strengthens non-El Niño wind …

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