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El Niņo and La Niņa
By
Karey Burek
I never understood the differences between El Niņo and La
Niņa, and why it affected the weather systems so much. I did some research and
this is what I came up with. El Niņo - As easterly trade winds decrease, warm water in the
western Pacific flows eastward. This layer, typically 500 feet deep flows over
cooler, nutrient rich water and blocks its normal upwelling along North and
South America. Sea life in these areas can suffer from lack of food. A great
example of this was off the coast of California in 1997. The mortality rate of
California sea lions in non El Niņo years is 25 percent. In 1997, the mortality
rate was 75 percent. This was due to the warm water rising to the top of the
ocean and sending the food sources (jellyfish, squid) to cooler water, which was
deeper and out of sea lion diving range. Another impact that El Niņo has on the
environment is on coral reefs. When the water becomes warmer, the reef expels
its algae and becomes white. Over time, the polyps eventually die. La Niņa - Pushed westward by strong trade winds, warm surface
water flows toward Asia. Colder deep-sea water upwells to the surface along the
Americas. Nutrients become more plentiful and evaporation decreases,
reducing storm cloud formation and rain in the region. Drought and colder than
normal temperatures are a result of La Niņa weather patterns. As you can see, both El Niņo and La Niņa affect our weather
and our environment. It influences food sources, animals, humans and the
weather. La Niņa - Pushed westward by strong trade winds, warm surface
water flows toward Asia. Colder deep-sea water rises to the surface along the
coast of the Americas. Nutrients become more plentiful and evaporation
decreases, reducing storm cloud formation and rain in the region. Drought and
colder than normal temperatures are a result of La Niņa weather patterns. As you can see, both El Niņo and La Niņa affect our weather
and our environment. It influences food sources, animals, humans and weather.
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