Effects of Hurricane Andrew in Florida
The effects of Hurricane Andrew in Florida proved to be at the time the costliest disaster in the state's history, as well as the then-costliest on record in the United States. Hurricane Andrew formed from a tropical wave on August 16, 1992 in the tropical Atlantic Ocean. It moved west-northwest and remained weak for several days due to strong wind shear. However, after curving westward on August 22, the storm rapidly intensified to reach peak winds of 175 mph (280 km/h). Following its passage through The Bahamas, Andrew made landfall near Homestead, Florida as a Category 5 hurricane on August 24. Eventually, Andrew struck southern Louisiana before it dissipated over the eastern United States on August 28.
Hurricane Arthur
Hurricane Arthur was the earliest known hurricane to make landfall in the U.S. state of North Carolina, and the first hurricane to make landfall in the United States since Hurricane Isaac in 2012. The first named storm of the 2014 Atlantic hurricane season, Arthur developed from an initially non-tropical area of low pressure over the Southeastern United States that emerged into the western Atlantic Ocean on June 28. After sufficiently organizing, developing a well-defined circulation and deep convection amid a favorable environment, it was classified a tropical depression on July 1. The system continued to strengthen, and was declared a tropical storm later that day. Drifting northward, the storm reached hurricane status early on July 3 and curved toward the north-northeast. Further structural organization resulted in additional intensification, and by 01:00 UTC on July 4, the system attained its peak winds of 100 mph (155 km/h) as a Category 2 hurricane on the Saffir–Simpson hurricane wind scale. Arthur made landfall at 03:15 UTC over North Carolina's Shackleford Banks, positioned between Cape Lookout and Beaufort, and intensified slightly further, with a minimum atmospheric pressure of 973 mbar (hPa; 28.70 inHg). The storm then trekked swiftly northeast, weakening as it passed by Cape Cod and Nantucket, before transitioning into an extratropical cyclone and coming ashore at Weymouth, Nova Scotia, on July 5. The remnants continued generally northeastward through Atlantic Canada before ultimately dissipating on July 9 over the Labrador Sea.