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Hurricane Diane was the costliest Atlantic hurricane of its time. One of three hurricanes to hit North Carolina during the 1955 Atlantic hurricane season, it formed on August 7 from a tropical wave between the Lesser Antilles and Cape Verde. Diane initially moved west-northwestward with little change in its intensity, but began to strengthen rapidly after turning to the north-northeast. On August 12, the hurricane reached peak sustained winds of 105 mph (170 km/h), making it a Category 2 hurricane. Gradually weakening after veering back west, Diane made landfall near Wilmington, North Carolina, as a strong tropical storm on August 17, just five days after Hurricane Connie struck near the same area. Diane weakened further after moving inland, at which point the United States Weather Bureau noted a decreased threat of further destruction. The storm turned to the northeast, and warm waters from the Atlantic Ocean helped produce record rainfall across the northeastern United States. On August 19, Diane emerged into the Atlantic Ocean southeast of New York City, becoming extratropical two days later and completely dissipating by August 23. The first area affected by Diane was North Carolina, which suffered coastal flooding but little wind and rain damage. After the storm weakened in Virginia, it maintained an area of moisture that resulted in heavy rainfall after interacting with the Blue Ridge Mountains, a process known as orographic lift. Flooding affected roads and low-lying areas along the Potomac River. The northernmost portion of Delaware also saw freshwater flooding, although to a much lesser extent than adjacent states. Diane produced heavy rainfall in eastern Pennsylvania, causing the worst floods on record there, largely in the Poconos and along the Delaware River. Rushing waters demolished about 150 road and rail bridges and breached or destroyed 30 dams. The swollen Brodhead Creek virtually submerged a summer camp, killing 37 people. Throughout Pennsylvania, the disaster killed 101 people and caused an estimated $70 million in damage (1955 USD). Additional flooding spread through the northwest portion of neighboring New Jersey, forcing hundreds of people to evacuate and destroying several bridges, including one built in 1831. Storm damage was evident but less significant in southeastern New York. Damage from Diane was heaviest in Connecticut, where rainfall peaked at 16.86 in (428 mm) near Torrington. The storm produced the state's largest flood on record, which effectively split the state into two by destroying bridges and cutting communications. All major streams and valleys were flooded, and 30 stream gauges reported their highest levels on record. The Connecticut River at Hartford reached a water level of 30.6 ft (9.3 m), the third highest on record there. The flooding destroyed a large section of downtown Winsted, much of which was never rebuilt. Record-high tides and flooded rivers heavily damaged Woonsocket, Rhode Island. In Massachusetts, flood water levels surpassed those during the 1938 Long Island hurricane, breaching multiple dams and inundating adjacent towns and roads. Throughout New England, 206 dams were damaged or destroyed, and about 7,000 people were injured. Nationwide, Diane killed at least 184 people and destroyed 813 houses, with another 14,000 homes heavily damaged. Monetary losses totaled $754.7 million, although the inclusion of loss of business and personal revenue increased the total to over $1 billion. In the hurricane's wake, eight states were declared federal disaster areas, and the name Diane was retired. ==Meteorological history== Hurricane Diane originated in a tropical wave first observed as a tropical depression on August 7 between the Lesser Antilles and Cape Verde. The system moved generally to the west-northwest, intensifying into a tropical storm on August 9. By the time the Weather Bureau first classified the storm on August 10, Diane was south of the Bermuda high, a semi-permanent ridge in the jet stream just east of Nova Scotia. Ships in the region of the storm reported winds of . During the next day, the Hurricane Hunters reported no increase in strength, and Diane initially remained disorganized.〔 The storm interacted with Hurricane Connie to its northwest in a process known as the Fujiwhara effect, in which Diane turned toward the north. Quick intensification ensued, potentially due to interaction with a cold-core low that increased atmospheric instability.〔 On August 12, the storm rapidly intensified into a hurricane.〔 The intensification was so quick that a ship southeast of the center believed Diane was undergoing a loop due to a steady drop in barometric pressure, despite moving away from the hurricane.〔 At its peak, Diane developed a well-defined eye about in diameter, described by reconnaissance aircraft as taking the shape of an "inverted teacup". The strongest winds were located in the northeast quadrant, where there was a secondary pressure minimum located northeast of the eye.〔 After moving to the north for about a day, Diane resumed its westward motion on August 13, after Hurricane Connie to the northwest had weakened. That day, Diane reached its lowest pressure of ,〔 and peak winds of 105 mph (170 km/h); originally the hurricane was analyzed to reach peak winds of 120 mph (195 km/h), although the large size and slow forward speed suggested the lower winds. It maintained its peak winds for about 12 hours, after which it weakened due to cooler air in the region. By August 15, the eye had become poorly defined, and winds steadily weakened. As it approached land, its center deteriorated, with minimal precipitation near the center; the eye was observed on a radar installed in July 1955. On August 17, Diane made landfall on the coast of North Carolina near Wilmington.〔 Pressure at landfall was estimated at , accompanied by winds just under hurricane intensity. Diane struck the state only five days after Hurricane Connie struck the same general area.〔 Diane quickly weakened as a tropical storm over the mountainous terrain of central North Carolina.〔 The associated area of precipitation expanded and spread away from the center to the north and northeast. The weakening system turned to the north and recurved toward the northeast through Virginia after a ridge built in from the west. It did not interact much with the non-tropical westerlies, and as a result it remained a distinct tropical cyclone over land. Convection redeveloped as the storm approached the Atlantic coast once again.〔 Diane passed through the Mid-Atlantic states, exiting New Jersey on August 19 into the Atlantic Ocean southeast of New York City. Paralleling the southern coast of New England, the storm later accelerated east-northeastward, becoming extratropical on August 21. Passing south and east of Newfoundland, the remnants of Diane accelerated and restrengthened slightly while moving to the northeast. Late on August 23, the storm dissipated between Greenland and Iceland.〔 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Hurricane Diane」の詳細全文を読む スポンサード リンク
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