Hurricane Irene was primarily caused by a combination of warm ocean waters, favorable atmospheric conditions, and the presence of low-pressure systems. In August 2011, these factors converged, allowing the storm to develop and intensify as it moved westward across the Atlantic Ocean. The warm waters provided the necessary energy for the hurricane, while atmospheric conditions, including light winds aloft, facilitated its growth and organization. Irene ultimately became a significant storm, impacting several regions along the East Coast of the United States.
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