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A low pressure system over warm ocean water will draw in warm moist air, causing convection to develop within the low, triggering thunderstorms fueled by this air. The convection lowers the pressure even further, causing the system to draw in even more warm, moist air, which further strengthens the convection. As the system strengthens in this manner the air in it starts to spin as a consequence of earth's rotation. This causes the convection to organize, allowing it to build more efficiently, allowing the storm to intensify even faster. As the storm strengthens the wind speed picks up and the storm continues to become better organized. When the winds hit 39 mph the system is considered a tropical storm, when they hit 74 mph it is considered a hurricane. Around this point the storm is usually spinning so fast that winds cannot reach all the way to the center of rotation, creating a calm area called the eye. If the storm strengthens further this feature will become better defined.

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Are hurricanes low pressure or high pressure?

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What pressure systems do hurricanes form around?

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Is a large swirling low-pressure system that forms over tropical waters?

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