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- Hurricane Beryl was a powerful and destructive Category 5 Atlantic hurricane that impacted several regions in late June and early July 2024. Here are the key details:
- 1. Formation and Intensity:
- - Beryl developed from a tropical wave that originated off the coast of Africa on June 25.
- - It rapidly intensified as it moved west through the central tropical Atlantic.
- - On July 1, Beryl made landfall on the island of Carriacou in Grenada as a high-end Category 4 hurricane, causing total devastation.
- - The hurricane intensified further as it entered the Caribbean Sea, peaking as a Category 5 hurricane with maximum sustained winds of 165 mph (270 km/h) and a minimum central pressure of 934 mbar (27.58 inHg).
- 2. Path and Impact:
- - Beryl caused catastrophic damage on Grenada's northern islands of Carriacou and Petite Martinique.
- - It also affected several other areas, including Saint Vincent and the Grenadines, Trinidad and Tobago, Venezuela, Jamaica, the Cayman Islands, and the Yucatán Peninsula.
- - After making landfall in Tulum, Quintana Roo (Mexico), as a high-end Category 2 hurricane, Beryl weakened over the Yucatán Peninsula.
- - It reorganized into a Category 1 hurricane in the Gulf of Mexico before making its final landfall near Matagorda, Texas.
- 3. Dissipation:
- - Beryl gradually weakened over land as it accelerated to the northeast.
- - It became post-tropical over the state of Arkansas on July 9 and eventually dissipated over Ontario on July 11.
- As for how hurricanes typically die out:
- - Several factors contribute to their weakening:
- - Land Interaction: When a hurricane moves over land, it loses its primary energy source (warm ocean water) and weakens.
- - Wind Shear: Strong winds at different altitudes can disrupt the hurricane's structure and reduce its strength.
- - Cooler Waters: Hurricanes thrive in warm waters; cooler waters lead to gradual weakening.
- - Dry Air Intrusion: Dry air entering the storm disrupts its convection and weakens it.
- - Topography: Mountains can disrupt the circulation and cause rapid weakening.
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