El Nino
Researcher: Kuchumbi Hayden
Mentor: Dr. Waldo Rodriguez
Center for Materials Research, NSU
A culmination of interactions between the ocean and the atmosphere, El Nino is
the anomalous warming of the southward countercurrent of waters in the eastern
equatorial Pacific Ocean, around the western coast of Peru and Ecuador.
Normally, the water of this region is cold, rich in nutrients, and flows
northward. The Southern Oscillation, a change in the surface pressure between
the southeastern Pacific and the western Pacific Ocean,is closely associated
with El Nino. Scientists give this relationship the name ENSO, El Nino-Southern
Oscillation. Usually, the surface pressure in the southeastern Pacific is much
higher that the pressure in the western Pacific Ocean. This differnce in
surface pressure creates a sharp pressure gradient which, facilitated by strong
westward trade winds, carries water currents from east to west. During El Nino,
the difference in the surface pressure between the eastern and western Pacific
Ocean decreases, thus diminishing the pressure gradient, and sometimes, even
switching the regions of high and low pressure in the ocean. When the surface
pressure of the western Pacific Ocean becomes higher that the surface pressure
in the east, water currrents move from the high pressure region to the low
pressure region, from west to east. With the reduced pressure difference in the
ocean come weaker trade winds that allow for the eastward movement of the
water currents. The overall result is warmer than normal waters in the eastern
Pacific, bringing about climatic differences both in areas around the Pacific
Ocean and around the world. The worldwide effects El Nino mark the importance
of study and research in this area. The eastward shift of warm waters in the
Pacific Ocean bring about increased precipitation in western parts of South
America and the United States and droughts in the eastern parts of Asia and
Australia. Adverse effects of El Nino due to increased precipitation and droughts
include flooding, property damage, brush fires, and crop failures. Careful
examination of the various aspects of El Nino will enable both a deeper
understanding of this phenomenon an dmore effective measures to prevent disasters.
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