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Jul 31st, 2024
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  1. 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:
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  3. 1. Formation and Intensity:
  4. - Beryl developed from a tropical wave that originated off the coast of Africa on June 25.
  5. - It rapidly intensified as it moved west through the central tropical Atlantic.
  6. - On July 1, Beryl made landfall on the island of Carriacou in Grenada as a high-end Category 4 hurricane, causing total devastation.
  7. - 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).
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  9. 2. Path and Impact:
  10. - Beryl caused catastrophic damage on Grenada's northern islands of Carriacou and Petite Martinique.
  11. - It also affected several other areas, including Saint Vincent and the Grenadines, Trinidad and Tobago, Venezuela, Jamaica, the Cayman Islands, and the YucatΓ‘n Peninsula.
  12. - After making landfall in Tulum, Quintana Roo (Mexico), as a high-end Category 2 hurricane, Beryl weakened over the YucatΓ‘n Peninsula.
  13. - It reorganized into a Category 1 hurricane in the Gulf of Mexico before making its final landfall near Matagorda, Texas.
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  15. 3. Dissipation:
  16. - Beryl gradually weakened over land as it accelerated to the northeast.
  17. - It became post-tropical over the state of Arkansas on July 9 and eventually dissipated over Ontario on July 11.
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  19. As for how hurricanes typically die out:
  20. - Several factors contribute to their weakening:
  21. - Land Interaction: When a hurricane moves over land, it loses its primary energy source (warm ocean water) and weakens.
  22. - Wind Shear: Strong winds at different altitudes can disrupt the hurricane's structure and reduce its strength.
  23. - Cooler Waters: Hurricanes thrive in warm waters; cooler waters lead to gradual weakening.
  24. - Dry Air Intrusion: Dry air entering the storm disrupts its convection and weakens it.
  25. - Topography: Mountains can disrupt the circulation and cause rapid weakening.
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