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Where low pressure is persistent, air is always converging and rising. When air rises, it often cools to its dewpoint to condense into clouds and precipitation.

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Q: Why is precipitation heavier in the persistent low pressure zones of the world?
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Related questions

Why is precipitation heavier in the presistent low-pressure zones of the world?

Low barometric pressure usually indicates that air is flowing upwards. When air moves upwards it cools and the moisture in it may condense to form clouds and possibly produce rain and thunderstorms.


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