Meteorological History
An area of disturbed weather in association with a weak surface trough and a stronger upper-level trough between the Bahamas and Bermuda developed on September 6. High pressure ridging strengthened by Tropical Storm Fay caused the trough to become more organized and close off into a broad non-tropical low on September 7. By September 8, the system had developed enough convection near its center of circulation to be classified Subtropical Depression Eight while located southeast of Cape Hatteras, North Carolina. Later that day, data from a Hurricane Hunter reconnaissance aircraft indicated that the system had strengthened into a subtropical storm, and the depression was upgraded to Subtropical Storm Gustav.
Gustav moved erratically to the west-northwest toward the North Carolina-South Carolina border over the next two days, it slowly strengthened, acquiring more tropical characteristics. On September 10, a poorly organized band of stronger winds developed around the center, and Gustav was designated a fully tropical storm shortly before turning toward the north and brushing Cape Hatteras, then accelerating toward the northeast and away from the coast. On September 11, while under the influence of a non-tropical system over New England, Gustav quickly strengthened into a hurricane, in a process similar to the intensification of Hurricane Michael in 2000. Gustav reached its peak intensity of 100 mph (160 km/h) later that day.
The hurricane began to slowly weaken and lose tropical characteristics on early September 12 as it moved over colder waters and encountered increasing wind shear. However, the storm was moving quickly enough to make landfall over Cape Breton, Nova Scotia as a Category 1 hurricane on September 12. Later that morning, Gustav made a second landfall in Newfoundland and became extratropical shortly after. The extratropical low continued moving slowly to the northeast before dissipating over the Labrador Sea on September 15.
Read more about this topic: Hurricane Gustav (2002)
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