Hurricane Grace was a short-lived Category 2 The Saffir–Simpson Hurricane Scale is a classification used for some Western Hemisphere tropical cyclones that exceed the intensities of tropical depressions and tropical storms. The scale divides hurricanes into five categories distinguished by the intensities of their sustained winds. In order to be classified as a hurricane, a tropical hurricane that contributed to the formation of the powerful 1991 "Perfect Storm". Forming on October 26, Grace initially had subtropical origins A subtropical cyclone is a weather system that has some characteristics of a tropical and an extratropical cyclone. As early as the 1950s, meteorologists were unclear whether they should be characterized as tropical or extratropical cyclones. They were officially recognized by the National Hurricane Center in 1972. Subtropical cyclones began to, meaning it was partially tropical A tropical cyclone is a storm system characterized by a large low-pressure center and numerous thunderstorms that produce strong winds and heavy rain. Tropical cyclones feed on heat released when moist air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic and partially extratropical Extratropical cyclones, sometimes called mid-latitude cyclones or wave cyclones, are a group of cyclones defined as synoptic scale low pressure weather systems that occur in the middle latitudes of the Earth having neither tropical nor polar characteristics, and are connected with fronts and horizontal gradients in temperature and dew point in nature. It became a tropical cyclone on October 27, and ultimately peaked with winds of 100 mph (155 km/h). The storm had minor effects on the island of Bermuda Bermuda is a British overseas territory in the North Atlantic Ocean. Located off the east coast of the United States, its nearest landmass is Cape Hatteras, North Carolina, about 1,030 kilometres (640 mi) to the west-northwest. It is about 1,373 kilometres (853 mi) south of Halifax, Nova Scotia, Canada, and 1,770 kilometres (1,100 mi) northeast of as it passed to the south. A developing extratropical storm to the north turned Grace eastward; the hurricane was eventually absorbed into the large circulation of the larger low pressure system. Fed by the contrast between cold air to the northwest and warm air from the remnants of Hurricane Grace, this storm became a large and powerful nor'easter that caused extremely high waves and resulted in severe coastal damage along the U.S. East Coast. (more...)
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