Meteorological History
A surface trough of low pressure with an area of convection persisted off the southeast coast of the United States on September 18. On the same day, a weak tropical wave which moved off the coast of Africa on September 8 approached the area. A cold front merged with the stationary area of disturbed weather on September 20, and on September 22 a circulation developed 200 miles (325 km) southeast of Cape Hatteras, North Carolina. Organization continued as outflow became better defined, and the system developed into Tropical Depression Six later that day.
The depression rapidly organized and attained tropical storm status with winds of 50 mph (80 km/h) just six hours after forming, upon which it was named Danielle. In response to an approaching trough, Danielle initially moved to the northeast. However, the trough outran the system, and a developing high pressure system to its north resulted in Danielle executing a tight, anticyclonic loop on September 23 to the 24th. The storm strengthened as it turned to the northwest, and reached a peak of 65 mph (105 km/h) winds on September 25 while just off the northeastern coast of North Carolina. Danielle turned to the north-northwest, and made landfall on the Eastern Shore of Virginia late on the 25th. It rapidly weakened over land, and dissipated over eastern Pennsylvania on September 26.
Read more about this topic: Tropical Storm Danielle (1992)
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