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Topic: |
Science
|
Number of pages / Number of words: |
5 / 1143 |
Essay's paper body
Where the
surface water moves away, colder, nutrient-rich water comes up from below to
replace it which is called upwelling. The winds that blow along the equator also
affect the properties of upwelled water. When there is no wind, the dividing
layer between the warm surface water and the deep cold water would be almost
flat; but the winds drag the surface water westward, raising the thermocline
nearly all the way up to the surface in the east and depressing in the west...
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When the easterlies are blowing at full strength, the upwelling of cold
water along the equatorial Pacific chills the air above it, making it too dense
to rise high enough for water vapor to condense to form clouds and raindrops. As
a result, this part of the ocean stays indubitably free of clouds during normal
years and the rain in the equatorial belt is mostly confined to the extreme
western Pacific...
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General points of the essay
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