Meteorological history | |
---|---|
Formed | September 8,1967 |
Dissipated | September 21,1967 |
Category 2 hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 100 mph (155 km/h) |
Lowest pressure | 973 mbar (hPa);28.73 inHg |
Overall effects | |
Fatalities | 3 |
Damage | $150,000 (1967 USD) |
Areas affected | East Coast of the United States |
IBTrACS | |
Part of the 1967 Atlantic hurricane season |
Hurricane Doria was an unusual and erratic hurricane that existed during September 1967. The fourth named storm and hurricane of the 1967 Atlantic hurricane season,Doria developed on September 8 off the east coast of Florida. It meandered until attaining tropical storm status,at which point the storm accelerated towards the northeast. On September 10,Doria intensified into a Category 2 hurricane on the modern-day Saffir–Simpson Hurricane Scale. After moving out to sea,the storm turned westward towards the United States. A compact cyclone,Doria weakened to a tropical storm shortly before moving ashore in the Mid-Atlantic States. The storm ultimately dissipated on September 21.
The storm,which ultimately made landfall near the Virginia–North Carolina border,produced high winds along the coast from New Jersey through North Carolina. A small boat sank off the coast of New Jersey,killing three of its occupants. Overall damage was estimated around $150,000 (1967 USD),although the storm overall was considered beneficial.
The origins of Hurricane Doria are traced back to an area of disturbed weather off the northeastern coast of Florida on September 4. For several days, the low pressure system meandered as its central barometric pressure gradually fell. [1] The storm is estimated to have organized into a tropical depression at 0000 UTC on September 8. [2] At the time, it was situated north of Grand Bahama Island. Drifting westward, the cyclone attained tropical storm intensity early the next day. [1] Doria turned northeastward and accelerated as it moved away from Florida. On September 10, the tropical storm achieved hurricane force. [2] Cold air became entrained into the hurricane's circulation by September 11, causing it to weaken to a tropical storm. However, its forward motion slowed and it once again strengthened. [1]
The hurricane moved eastward, seemingly out to sea. However, an area of high pressure over New England began to steer Doria westward on September 13. [3] The hurricane continued to strengthen, and it is estimated to have peaked with maximum sustained winds of 100 mph (155 km/h) and a minimum air pressure of 973 mbar (hPa; 28.73 inHg). It maintained these winds for approximately 18 hours, before weakening slightly late on September 14. [2] In his 2007 book "Hurricanes and the Middle Atlantic States", Rick Schwartz compared Doria to the 1933 Chesapeake–Potomac hurricane, citing similar intensities, tracks, and forward speeds. [3] On September 16, the storm weakened to a tropical storm in a colder, drier environment. As it turned southward, Doria quickly weakened. [1] Initial forecasts suggested the possibility for the storm to maintain its severity and move ashore between Maryland and New Jersey. [3]
Continually deteriorating, Doria made landfall near the Virginia–North Carolina border, and moved south over land. It reemerged over open waters on September 17, and at around the same time, it weakened to a tropical depression. It curved southeastward as a weak depression, and several days later it was still identifiable as a storm system south of the island of Bermuda. [1] It dissipated on September 21. [2] Doria had an unusual and capricious track, described as "one of the most erratic storms ever observed". [1]
In advance of the storm, hurricane warnings were issued for much of the East Coast of the United States. For 19 hours, about 260 mi (420 km) of shoreline was under an advisory. [4] At least 400 people were evacuated from their homes in southern New Jersey and 6,600 from Ocean City, Maryland. [5]
Doria was a small storm, [3] although it brought high winds and moderate coastal flooding to some areas; [6] generally light rainfall was also observed. In North Carolina, 6.09 in (155 mm) of precipitation fell at Whiteville. [7] Flash flooding and the overflowing of storm sewers ensued in the southeastern portions of the state; there were also losses to crops, especially corn, cotton, and tobacco. [8] In Virginia, strong winds were reported along the coast, with gusts up to 60 mph (97 km/h) at Wallops Island. [1] Along the east coast of the state, winds damaged trees, roofs, signs, and billboards. In Maryland, similar impact occurred in Ocean City, with damage sustained to signs and billboards and tore the roof of a prefabricated home; [9] a city boardwalk also sustained storm-related damage. [4]
A station at the Indian River Inlet in Delaware recorded a tide 6.5 ft (2.0 m) above-normal; the highest sustained winds reported on land association with the storm, 50 mph (80 km/h), also occurred there. [1] Atlantic City, New Jersey, recorded a peak gust of 39 mph (63 km/h), with rainfall amounting to 0.53 in (13 mm). Damage from the storm was generally light. Off the coast of Ocean City, New Jersey, a cabin cruiser sank in 25-ft (7.6 m) seas. [1] [4] Three of the vessel's occupants, a mother and her two sons, drowned. [10] In Massachusetts, some small boats sank at the harbors. At Ipswich Bay, 10 people required rescue after two boats capsized. Minor beach erosion was reported at Nantucket. [8] Overall damage was estimated at $150,000, which was considered minor. The storm's passage was considered beneficial, due to adding sand to beaches and providing favorable rains. [11]
The 1959 Atlantic hurricane season featured near normal tropical cyclone activity overall. The season officially began on June 15, 1959 and lasted until November 15, 1959. These dates historically described the period in each year when most tropical cyclogenesis occurs in the Atlantic basin. However, the formation of a tropical cyclone is possible at any time of the year, as shown in 1959, by the formation of Tropical Storm Arlene on May 28. Arlene struck Louisiana and brought minor flooding to the Gulf Coast of the United States. The next tropical storm, Beulah, formed in the western Gulf of Mexico and brought negligible impact to Mexico and Texas. Later in June, an unnamed hurricane, caused minor damage in Florida, and then devastated parts of Maritime Canada, resulting in what became known as the Escuminac disaster. Hurricane Cindy brought minor impact to The Carolinas. In late July, Hurricane Debra produced flooding in the state of Texas. Tropical Storm Edith in August and Hurricane Flora in September caused negligible impact on land.
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The 1963 Atlantic hurricane season It was a slightly below average season in terms of tropical cyclone formation, with a total of ten nameable storms. Even so, it was also a notoriously deadly and destructive season. The season officially began on June 15, 1963, and lasted until November 15, 1963. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first system, an unnamed tropical storm, developed over the Bahamas on June 1.
The 1966 Atlantic hurricane season saw the Weather Bureau office in Miami, Florida, be designated as the National Hurricane Center (NHC) and assume responsibility of tropical cyclone forecasting in the basin. The season officially began on June 1, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was an above-average season in terms of tropical storms, with a total of 15. The first system, Hurricane Alma, developed over eastern Nicaragua on June 4 and became the most recent major hurricane in the month of June. Alma brought severe flooding to Honduras and later to Cuba, but caused relatively minor impact in the Southeastern United States. Alma resulted in 90 deaths and about $210.1 million (1966 USD) in damage.
The 1967 Atlantic hurricane season was an active Atlantic hurricane season overall, producing 13 nameable storms, of which 6 strengthened into hurricanes. The season officially began on June 1, 1967, and lasted until November 30, 1967. These dates, adopted by convention, historically describe the period in each year when most tropical cyclogenesis occurs in the Atlantic Ocean. The season's first system, Tropical Depression One, formed on June 10, and the last, Tropical Storm Heidi, lost tropical characteristics on November 2.
The 1968 Atlantic hurricane season was a below average hurricane season during which only nine nameable storms developed. The season officially began on June 1 and lasted until November 30, dates which conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. Of the named storms, five strengthened into hurricanes; none however intensified into a major hurricane. Only four other seasons since the start of the satellite era—1972, 1986, 1994, and 2013—did not feature a major hurricane. The first system, Hurricane Abby, developed in the northwestern Caribbean on June 1. Abby moved northward and struck Cuba, bringing heavy rainfall and flooding to western portions of the island. Making landfall in Florida on June 4, Abby caused flooding and spawned four tornadoes, but left behind little damage. Overall, the hurricane resulted in six deaths and about $450,000 (1968 USD) in damage. In late June, Tropical Storm Candy brought minor flooding and spawned several tornadoes across portions of the Southern United States. Overall damage from the cyclone reached approximately $2.7 million. 1968 featured two simultaneously active tropical storms during the month of June, a phenomenon that would not occur again until 2023.
The 1969 Atlantic hurricane season was the most active Atlantic hurricane season since the 1933 season, and was the final year of the most recent positive ("high-quality") Atlantic multidecadal oscillation (AMO) era. The hurricane season officially began on June 1, and lasted until November 30. Altogether, 12 tropical cyclones reached hurricane strength, the highest number on record at the time; a mark not surpassed until 2005. The season was above-average despite an El Niño, which typically suppresses activity in the Atlantic Ocean, while increasing tropical cyclone activity in the Pacific Ocean. Activity began with a tropical depression that caused extensive flooding in Cuba and Jamaica in early June. On July 25, Tropical Storm Anna developed, the first named storm of the season. Later in the season, Tropical Depression Twenty-Nine caused severe local flooding in the Florida Panhandle and southwestern Georgia in September.
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The 1972 Atlantic hurricane season was a significantly below average season, having only seven named storms, four fully tropical storms and three subtropical storms. It officially began on June 1, 1972, and lasted until November 30, 1972. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, Subtropical Storm Alpha, developed on May 23 off the Southeast United States and struck Florida, causing minor damage and two fatalities.
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