Exact(16)
The typhoon began forming on November 2 as an area of convection located in the equatorial Pacific Ocean some 230 nautical miles east-southeast of Pohnpei island in the Federated States of Micronesia.
The typhoon began as an area of convection located in the equatorial Pacific Ocean some 230 nautical miles (425 km) east-southeast of Pohnpei on November 2. Later that day, the Joint Typhoon Warning Center (JTWC) at Pearl Harbor, Hawaii, reclassified the disturbance as a tropical depression, naming the storm Tropical Depression 31W.
The simulated sea surface cooling induced by the typhoon began to have an impact on the simulated central pressure during the intensification phase for all four typhoons.
Shortly thereafter, the typhoon began to weaken as it approached the Philippines.
The typhoon began to become extratropical after making landfall, and continued northeastward through southern China.
During the night of May 18, the typhoon began to weaken.
Similar(44)
Safe and warm, he flips from Bush's speech to the National Geographic channel, a favorite of his, as the typhoon begins to roar.
With winds of 90 miles per hour and gusts of up to 112 miles per hour, Typhoon Sinlaku began to pound northeastern Taiwan.
Typhoon Pat began to accelerate in the direction of Japan.
The outer bands of Typhoon Wipha began impacting parts of eastern China on September 17.
The forward motion on the typhoon also began to increase as it interacted with a baroclinic zone.
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