Coriolis force and pressure gradient force around a low pressure region
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The combined effects of the Coriolis and the Pressure gradient forces cause the winds. The winds blow around pressure areas parallel to the isobars. ... In Low pressure zones, winds converge and ascend, spiraling upward to form a cyclone (counterclockwise in the Northern Hemisphere).
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The combined effects of the Coriolis and the Pressure gradient forces cause the winds. The winds blow around pressure areas parallel to the isobars. ... In Low pressure zones, winds converge and ascend, spiraling upward to form a cyclone (counterclockwise in the Northern Hemisphere).
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