Tropical Storm Danielle (1992)
| Tropical storm (SSHWS/NWS) | |
Tropical Storm Danielle off the coast of North Carolina
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| Formed | September 22, 1992 |
|---|---|
| Dissipated | September 26, 1992 |
| Highest winds |
1-minute sustained: 65 mph (100 km/h) |
| Lowest pressure | 1001 mbar (hPa); 29.56 inHg |
| Fatalities | 2 direct |
| Areas affected | North Carolina, Virginia, Maryland, Delaware, New Jersey, Pennsylvania |
| Part of the 1992 Atlantic hurricane season | |
Tropical Storm Danielle was a strong tropical storm that made landfall on Virginia in the 1992 Atlantic hurricane season. The fourth storm of the season, Danielle was one of two tropical cyclones in the year to make landfall in the United States, the other being Hurricane Andrew. It formed out of a stationary trough of low pressure on September 18 near the coast of North Carolina. The system quickly reached tropical storm status, and Danielle looped to the west due to a change in steering currents. Tropical Storm Danielle reached a peak of 65 mph (105 km/h) winds before weakening and hitting the Delmarva Peninsula. The storm quickly dissipated over land.
The storm dropped light rainfall throughout its path, and winds were minimal. The combination of Danielle and a high pressure system produced higher than normal tides and strong waves, causing beach erosion and light coastal damage. The waves killed two in New Jersey from a boat sinking, and also destroyed three houses in the Outer Banks of North Carolina. Overall damage from the storm was minimal.
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.
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