What is El Niño and what causes one?
The waters of the eastern Pacific Ocean
are heating
up, scientists say, building towards a strong El Niño event
that could rival the intensity of the record 1997 event that wreaked
weather-related havoc across the globe, from mudslides in California to
fires in Australia.
According to the
latest forecast released Thursday by NOAA's Climate Prediction Center,
this year's El Niño is "significant and strengthening."
"There
is a greater than 90% chance that El Niño will continue through
Northern Hemisphere winter 2015-16, and around an 85% chance it will
last into early spring 2016," the NOAA said in a statement.
The
weather phenomenon largely became a part of the public vernacular
during the 1997 El Niño. It caused devastating flooding in the western
U.S. and drought in Indonesia. It was blamed for deadly virus outbreaks
in Africa and rising coffee prices around the world.
Chris Farley became El Niño personified on Saturday Night Live.
Pure chaos. But what is El Niño, and what impact will it have this time around? Let us explain.
El
Niño is a warming of the eastern Pacific Ocean, mainly along the
Equator -- see the thick red belt in the satellite photo, which
indicates waters that are warmer than normal.
These
warmer waters are normally confined to the western Pacific by winds
that blow from east to west, pushing the warmer water toward Indonesia
and Australia.
But during an El Niño,
the winds slow down and can even reverse direction, allowing the warmer
water to spread eastward all the way to South America.
El
Niños occur every two to seven years in varying intensity, and the
waters of the eastern Pacific can be up to 4 degrees Celsius (7 degrees
Fahrenheit) warmer than usual.
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