Hurricanes in the northern Atlantic occur primarily during the warm summer and early fall months when ocean temperatures rise above 26.5°C (about 80°F). Warm ocean water serves as fuel for the storms, allowing them to gain strength and energy. Additionally, the Coriolis effect, caused by the Earth's rotation, helps to organize and spin the storms, leading to their development. Atmospheric conditions, such as low wind shear and moisture in the upper levels of the atmosphere, also contribute to hurricane formation.
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