Climate Change - Macro Scale. What is the Walker Cell?

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Climate Change – Macro Scale

What is the Walker Cell?

This is the normal atmospheric conditions in the Pacific Ocean.  The great NE and SE trade wind belts blow equatorward and westward across the width of the Pacific towards the warm water of the west.  A convectional uplift occurs as the water heats up.  Pressure rises over the eastern Pacific Ocean, off the coast of South America, and falls over the western Pacific Ocean, toward Indonesia and the Philippines.  The descending air in the east gives the clear, dry conditions that create the Atacama Desert in Peru, whilst the warm, moist air ascending in the west gives heavy convectional rainfall. 

What are the atmospheric conditions in an El Nino year?

During an El Nino year the normal conditions are reversed in the equatorial Pacific region, in pressure, precipitation and often in winds and ocean currents.  Pressure rises over the western Pacific and falls over the eastern Pacific causing the region of rising air to move east with the associated convectional uplift.  This allows the ITCZ to migrate southwards and cause the trade winds to weaken in strength, or even to be reversed in direction.  The descending air gives much direr conditions in South-east Asia, than it usually experiences and on extreme conditions even causing drought.  In the eastern Pacific air is now rising, giving much wetter conditions in places like Peru, that normally experience desert like conditions.  The change in direction of the trade winds means that: surface water tend to be pushed eastwards so that sea-level in South-east Asia falls, whilst rises in South America; and surface water temperatures in excess of 28ºC extend much further eastwards and the upwelling of cold water off South America is reduced allowing sea temperatures to rise by 6ºC.  This warmer water in the eastern Pacific lacks oxygen, nutrients and therefore plankton, having an adverse affect on Peru’s fishing industry.  

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What do the “normal” trade winds do for the area?

In the Walker Cell they: push water westwards so that the level in the Philippines is normally 60sm higher than Panama and Columbia; allow water, flowing westward as the equatorial current, to remain near to the ocean surface where it can gradually heat (giving the world’s highest ocean temperatures - 28ºC).  In contrast, as warm water is pushed away from South America it is replaced by an upwelling of colder, nutrient-rich water.  Although this water lowers temperatures below 20ºC, it does provide a plentiful supply of plankton, which forms the ...

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