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December 1992 nor'easter
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December 1992 nor'easter : ウィキペディア英語版
December 1992 nor'easter

The December 1992 nor'easter produced record high tides and snowfall across the northeastern United States. It developed as a low pressure area on December 10 over Virginia, and for two days it remained over the Mid-Atlantic states before moving offshore. In Maryland, the snowfall unofficially reached ; if verified, the total would have been the highest in the state's history. About 120,000 people were left without power in the state due to high winds. Along the Maryland coast, the storm was less severe than the Perfect Storm in the previous year, although the strongest portion of the storm remained over New Jersey for several days. In the state, winds reached in Cape May, and tides peaked at in Perth Amboy. The combination of high tides and waves caused the most significant flooding in the state since the Ash Wednesday Storm of 1962. Several highways and portions of the New York City Subway and Port Authority Trans-Hudson systems were closed due to the storm. Throughout New Jersey, the nor'easter damaged about 3,200 homes and caused an estimated $750 million in damage (1992 USD).
The nor'easter increased tides across the northeastern United States for several days due to its slow movement. In New York City, tides reached at Battery Park, which flooded Franklin D. Roosevelt East River Drive. Along Long Island, the nor'easter destroyed over 130 homes and left 454,000 people without power. In New England, 230,684 people lost power during the storm. Five houses were destroyed in Massachusetts, and flooding reached deep in Boston. Further inland, the storm produced significant snowfall, estimated at around in The Berkshires. The high snow totals closed schools for a week in western Massachusetts. Overall, the storm caused between $1–2 billion in damage (1992 USD) and 19 deaths, of which four were directly related to the storm. In March of the following year, the Storm of the Century caused worse damage across a larger region of the eastern United States.
==Meteorological history==
A storm complex moved eastward from the Texas coast into Georgia on December 9. On December 9, the National Weather Service (NWS) issued a coastal flood watch in anticipation of the developing storm. On December 10, an upper-level trough was located along the East Coast of the United States. At around 1200 UTC that day, cyclogenesis – the development of an low pressure area – occurred over southeastern Virginia.〔 The cyclone moved quickly northward through the Chesapeake Bay until reaching a position just west of Chestertown, Maryland on December 11.〔 By that time, the system had intensified to a pressure of ,〔 while the parent trough extended from Maryland through the New York metropolitan area to around Cape Cod.〔 On December 11, the NWS issued gale warnings and advised for boats to avoid the ocean.〔 The storm turned to the southeast and briefly stalled near Georgetown, Delaware.〔 This was due to a high pressure area north of Maine halting its motion. The interaction between the two systems produced strong easterly winds from Virginia to New England. The nor'easter finally moved offshore on December 12,〔 and later that day passed to the southeast of Long Island.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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