GS 1: Physical GeographyGS 3: Environment & EcologyGS 3: Disaster ManagementPrelims

Wind speeds of 280 kmph: What made Super Typhoon Ragasa so intense?, Pg 22.

Super Typhoon Ragasa devastates Hong Kong and Southern China with record-breaking 280 kmph winds, displacing millions and causing widespread damage.

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Key Highlights:

  • Super Typhoon Ragasa struck Hong Kong on Wednesday, forcing two million people in southern China to evacuate.
  • The typhoon had maximum sustained winds of 280 kmph, making it the most intense tropical cyclone recorded in 2025.
  • Ragasa has caused at least 14 deaths in Taiwan and 2 deaths in the northern Philippines.
  • Coastal waters in Hong Kong rose more than 3 meters due to a significant storm surge.

Detailed Insights:

  • Tropical cyclones form over warm ocean waters near the equator, gaining strength from the ocean's heat and evaporated water.
  • The Saffir-Simpson Hurricane Wind Scale categorizes cyclones based on maximum sustained wind speed, ranging from Category 1 (119-153 kmph) to Category 5 (252 kmph or higher).
  • The 'dirty' side of a tropical cyclone in the northern hemisphere, which is the right-hand side relative to its motion, experiences the most powerful winds due to the combination of the storm's forward motion and rotating circulation.
  • Rising global temperatures are believed to be intensifying tropical cyclones, with studies indicating that cyclones in Southeast Asia are forming closer to coastlines and intensifying more rapidly.
  • Warmer surface temperatures in the Pacific Ocean, where Ragasa formed, have risen by about 1.5 degrees Celsius in the past century, contributing to the typhoon's intensity.

Key Concepts Involved:

  • Tropical Cyclone: A rotating, organized system of clouds and thunderstorms that originates over tropical or subtropical waters and has a closed low-level circulation.
  • Saffir-Simpson Scale: A 1 to 5 rating based on a hurricane's sustained wind speed, estimating potential property damage.
  • Storm Surge: An abnormal rise in sea level during a tropical cyclone, caused primarily by the storm's winds pushing water onshore.
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