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Tropical Storm Alberto (2006)

Tropical Storm Alberto
Tropical storm (SSHWS/NWS)
Tropical storm alberto 2006.jpg
Tropical Storm Alberto near peak strength on June 12
Formed June 10, 2006
Dissipated June 14, 2006
Highest winds 1-minute sustained: 70 mph (110 km/h)
Lowest pressure 995 mbar (hPa); 29.38 inHg
Fatalities 3 indirect, 4 missing
Damage $420,000 (2006 USD)
Areas affected Northwest Caribbean, Southeastern United States, Atlantic Canada
Part of the 2006 Atlantic hurricane season

Tropical Storm Alberto was the first tropical storm of the 2006 Atlantic hurricane season. Forming on June 10 in the northwestern Caribbean, the storm moved generally to the north, reaching a maximum intensity of 70 mph (110 km/h) before weakening and moving ashore in the Big Bend area of Florida on June 13. Alberto then moved through eastern Georgia, North Carolina, and Virginia as a tropical depression before becoming extratropical on June 14.

Across the Western Caribbean, the storm produced heavy rainfall, causing some minor damage. In Florida, a moderate storm tide caused coastal damage and flooding, while Alberto's outer rainbands produced several tornadoes. The storm was indirectly responsible for two drownings off the coast of Tampa Bay. In North Carolina, heavy rainfall caused locally severe flooding, and one child drowned in a flooded storm drain near Raleigh. The remnants of Alberto produced strong winds and left four people missing in Atlantic Canada. Overall, damage was minor along Alberto's path.

In early June 2006, an area of convection persisted across Central America and the western Caribbean in association with a broad, nearly stationary trough of low pressure. Thunderstorms increased and became more concentrated on June 8 after a tropical wave moved into the western Caribbean, and an upper-level low to its west increased outflow over the system. The disturbance moved slowly north-northwestward, and development was initially inhibited by marginally favorable upper-level winds and land interaction. The system gradually organized, and by June 10 a circulation formed with sufficiently organized convection for the National Hurricane Center to classify it Tropical Depression One. At this point the storm was located about 140 miles (225 km) south of the western tip of Cuba.


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