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Precipitation
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generally increases in
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the areas of regional
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tropical precipitation
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maxima (such as the
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monsoon regimes) and
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over the tropical Pacific.
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Precipitation
generally
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decreases in the
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subtropics and increases
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at high latitudes è
due
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to the poleward shift of
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the storm track è due
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to the expansion of the
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Hadley circulation.
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