Seasonal variation in the number of hurricanes in the Atlantic is primarily influenced by warm ocean waters, atmospheric conditions, and wind patterns. The hurricane season typically peaks from August to October when sea surface temperatures are highest, providing the necessary heat and moisture for storm development. Additionally, reduced wind shear and favorable atmospheric conditions during this period facilitate the formation and strengthening of hurricanes. Climate phenomena, such as El Niño and La Niña, can also impact hurricane activity by altering oceanic and atmospheric dynamics.
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