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Hurricanes are powerful storms formed when moist air rises, creating low pressure. As this process continues, more moist air is drawn in, accelerating the storm's intensity. Cooler air is pulled downward, and the winds circulate counterclockwise in the Northern Hemisphere, particularly near the equator. As hurricanes progress, they gather more moisture, increasing their speed and potential for destruction. Understanding these dynamics is crucial for preparedness and safety during hurricane season.
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