Meteorological history | |
---|---|
Formed | September 13,1964 |
Dissipated | September 24,1964 |
Category 4 major hurricane | |
1-minute sustained (SSHWS/NWS) | |
Highest winds | 130 mph (215 km/h) |
Lowest pressure | 945 mbar (hPa);27.91 inHg |
Overall effects | |
Fatalities | 1 |
Damage | $100,000 (1964 USD) |
Areas affected | East Coast of the United States,Atlantic Canada |
IBTrACS | |
Part of the 1964 Atlantic hurricane season |
Hurricane Gladys was a tropical cyclone that caused minor impact along the East Coast of the United States,Bermuda,and Atlantic Canada. The ninth named storm and fifth hurricane of the 1964 Atlantic hurricane season,Gladys developed from a tropical wave located east of the Lesser Antilles on September 13. Shortly thereafter,it strengthened into a tropical storm. On September 14,Gladys abruptly intensified into a Category 2 hurricane on the Saffir–Simpson hurricane wind scale. However,early on the following day,Gladys weakened slightly to a Category 1 hurricane. Between late on September 16 and late on September 17,the storm rapidly strengthened,peaking as a 145 mph (233 km/h) Category 4 hurricane on the latter. Gladys began weakening on the following day and curved northward on September 19.
The storm turned northwestward on September 22 and briefly threatened the East Coast of the United States. However,it veered northeastward on September 23 and moved rapidly toward Atlantic Canada. By 0000 UTC on September 25,Gladys became extratropical while centered between Sable Island and Nova Scotia. Along the East Coast of the United States,Gladys produced light rainfall,gusty winds,and storm surge. Coastal flooding was reported in North Carolina and Virginia. In the former,high tides inundated homes and buildings with 2 feet (0.61 m) of water in two small villages on the Outer Banks and flooded a highway to Manteo. In the state of Virginia,one death occurred when a man was fatally struck in the throat by debris. Tides also effected the Mid-Atlantic,New England,and Atlantic Canada.
A tropical wave was first observed over western Africa on September 8 and moved offshore in the vicinity of Dakar, Senegal on the following day. [1] At 0600 UTC on September 13, a tropical depression developed while centered about halfway between Cape Verde and the Lesser Antilles. [2] Later that day, the S.S. Gerwi reported heavy rain and winds of 63 mph (101 km/h), [3] confirming the existence of Tropical Storm Gladys at 1200 UTC on September 13. [2] Four hours later, the Weather Bureau Office in San Juan, Puerto Rico initiated advisories on Gladys. A hurricane hunter plane flew into Gladys on the afternoon of September 13 was unable to obtain wind data due to darkness. [1] A reconnaissance flight into the storm on September 14 noted that it had strengthened into a hurricane, while moving west-northwestward at about 18 mph (29 km/h). [3] HURDAT records indicate that around that time, Gladys became a Category 2 hurricane as winds reached 100 mph (160 km/h). However, early on September 15, Gladys weakened slightly to a Category 1 hurricane. [2]
Early on September 17, the storm began to rapidly intensify. By 1800 UTC, Gladys attained its peak intensity with maximum sustained winds of 145 mph (233 km/h) and a minimum barometric pressure of 945 mbar (27.9 inHg ). The storm later began to weaken and fell to a Category 3 hurricane early on September 19. Around that time, Gladys curved northward in response to a weak trough in the westerlies. [3] Early on September 20, it further weakened to a Category 2 hurricane. [2] Rising atmospheric pressures to the north forced the storm to curve northwestward on September 21. [3] Later that day, Gladys weakened to a Category 1 hurricane. [2] The storm posed a threat to the East Coast of the United States, and passed about 140 miles (230 km) east of Cape Hatteras, North Carolina, before a deepening low pressure area over the Great Lakes region caused it to veer northeastward. [3] Gladys then accelerated and approached Atlantic Canada, before transitioning into an extratropical cyclone at 0000 UTC on September 25, while located between Nova Scotia and Sable Island. The extratropical remnants continued northeastward into Newfoundland and dissipated later on September 25. [2]
As Gladys strengthened in the Atlantic Ocean, forecasters at the United States Weather Bureau predicted that the storm would bring high surf to areas as far north as North Carolina. Additionally, it was suggested that Gladys could have threatened northern Florida, as the storm was on a similar path as Hurricane Dora earlier in the month. As a result, residents along the coast of the Southeastern United States were advised to remain alert and small craft advisories were issued. [4] [5] On September 20, small craft advisories were issued for The Bahamas. [6] After Gladys turned northwestward on September 21, forecasters at the United States Weather Bureau issued hurricane watches for North Carolina, Virginia, and some Mid-Atlantic states. [7] Gale warnings and small craft advisories were issued on September 23 from Massachusetts to Rhode Island. [8] In Rhode Island, ships of the United States Navy were diverted to Narragansett Bay as a precaution. [9] At 0400 UTC on September 24, the gale warnings for New England were lowered as Gladys turned northeastward away from the coast however, small water craft were advised to remain in port until the seas subsided. [10]
In the United States, Gladys produced high tides as far south as Florida and Georgia. [4] [6] Hurricane Gladys' effects on South Carolina was minimal as the center of the hurricane was a considerable distance from the coastline. The only effects Gladys was minor rainfall, peaking at 1 inch (25 mm) in Myrtle Beach, as well as storm tides of 2 feet (0.61 m) above normal along the upper coast of South Carolina. [11]
In North Carolina, the large wind field of Gladys produced tropical storm force winds near Manteo. Waves produced by the strong winds flooded a highway leading away from Manteo. [12] Between Kill Devil Hills and Nags Head, U.S. Route 158 was inundated by 2 feet (0.61 m) of water. [13] Near Cape Hatteras, a weather station recorded sustained winds of 40 mph (64 km/h) and gusts up to 41 mph (66 km/h). Additionally, tides in the area ranged from 2–2.5 feet (0.61–0.76 m) above normal. [12] The abnormal tides and heavy wave action flooded two small villages, leaving many homes and buildings under 2 feet (0.61 m) of water [9] and washed away grasses that were planted to stabilize the sand dunes. [12] In Wilmington, sustained winds of 25 mph (40 km/h) and gusts of 28 mph (45 km/h) were reported, [14] as well as tides 2–3 feet (0.61–0.91 m) above normal. [12] Elsewhere in the Outer Banks, high winds caused a mobile home to fall off its foundations and blew down two television antennas. [15]
A weather station in Norfolk, Virginia recorded gusts of 38–44 mph (61–71 km/h) and 0.17 inches (4.3 mm) of rainfall. In Cape Henry, sustained winds of 42 mph (68 km/h) and a precipitation total of 0.02 inches (0.51 mm) were reported. Coastal sections of southeastern Virginia experienced tides 2.2–6.1 feet (0.67–1.86 m) above normal, resulting in minor tidal flooding. [16] One indirect fatality was attributed from Gladys when a man suffered fatal wounds to his throat due to flying debris. [17] High winds and strong ocean currents from Gladys produced beach erosion in New Jersey, New York and Massachusetts. [18] In Rhode Island, the outer bands of Gladys produced light rainfall, peaking at 0.38 inches (9.7 mm). [19] A boy was washed into the sea by the waves offshore Narragansett and was rescued by United States Coast Guard servicemen, who dove into the water after two previous attempts to rescue him failed. [20]
Hurricane Gladys produced rough seas that affected Puerto Rico, the Virgin Islands, the northern Leeward Islands and the northern Bahamas. [4] [6] The outer bands of Gladys also lashed Bermuda with winds but little damage if any was reported. [9] In Atlantic Canada, Gladys passed over Newfoundland as a 70 mph (110 km/h) extratropical storm but no damage was reported. [2] At St. John's Harbor, 65 ships took shelter as a precaution. Some ships suffered damage, including two foreign freighters. [21]
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 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 1964 Atlantic hurricane season featured the highest number of U.S.-landfalling hurricanes since 1933. The season officially began on June 15, and lasted until November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The season was above average, with thirteen named storms, seven hurricanes, and five major hurricanes. The first system, an unnamed tropical storm, developed on June 2, almost two weeks before the official start of the season. Striking Florida on June 6, the storm brought localized flooding to portions of Cuba and the Southeastern United States, leaving about $1 million in damage. The next storm, also unnamed, developed near the end of July; it did not impact land.
The 1965 Atlantic hurricane season was the first to use the modern-day bounds for an Atlantic hurricane season, which are June 1 to November 30. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. It was a slightly below average season, with 10 tropical cyclones developing and reaching tropical storm intensity. Four of the storms strengthened into hurricanes. One system reached major hurricane intensity – Category 3 or higher on the Saffir–Simpson hurricane scale. The first system, an unnamed tropical storm, developed during the month of June in the southern Gulf of Mexico. The storm moved northward across Central America, but caused no known impact in the region. It struck the Florida Panhandle and caused minor impact across much of the Southern United States. Tropical cyclogenesis halted for over two months, until Anna formed on August 21. The storm remained well away from land in the far North Atlantic Ocean and caused no impact.
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The 1949 Atlantic hurricane season was the last season that tropical cyclones were not publicly labeled by the United States Weather Bureau. It officially began on June 15, and lasted until November 15. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. The first storm, a tropical depression, developed in the northern Gulf of Mexico on August 14. The final system, Tropical Storm Sixteen, dissipated in the southwestern Caribbean Sea on November 5. It was a fairly active season, featuring 16 tropical storms and seven hurricanes. Two of these strengthened into major hurricanes, which are Category 3 or higher on the Saffir–Simpson hurricane wind scale.
The 1947 Atlantic hurricane season was the first Atlantic hurricane season to have tropical storms labeled by the United States Air Force. The season officially began on June 16, 1947, and ended on November 1, 1947. These dates conventionally delimit the period of each year when most tropical cyclones form in the Atlantic basin. However, the first tropical cyclone developed on June 13, while the final system was absorbed by a cold front on December 1. There were 10 tropical storms; 5 of them attained hurricane status, while two became major hurricanes, which are Category 3 or higher on the modern day Saffir–Simpson scale. Operationally, the third tropical storm was considered two separate tropical cyclones, resulting in the storm receiving two names. The eighth tropical storm went undetected and was not listed in HURDAT until 2014.
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The 1905 Atlantic hurricane season featured five known tropical cyclones, two of which made landfall in the United States. The first system was initially observed near the Windward Islands on September 6. The last system to dissipate, the fourth storm, transitioned into an extratropical cyclone on October 11, while located well southeast of Newfoundland. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Between October 5 and October 10, the fourth and fifth system existed simultaneously.
The 1901 Atlantic hurricane season was the most active season without a major hurricane – tropical cyclones that reach at least Category 3 on the Saffir–Simpson hurricane wind scale – until 2013. The first system was initially observed in the northeastern Caribbean on June 11. The fourteenth and final system transitioned into an extratropical cyclone near Bermuda on November 5. These dates fall within the period with the most tropical cyclone activity in the Atlantic. Eight of the fourteen tropical cyclones existed simultaneously.
The 1899 Atlantic hurricane season featured the longest-lasting tropical cyclone in the Atlantic basin on record. There were nine tropical storms, of which five became hurricanes. Two of those strengthened into major hurricanes, which are Category 3 or higher on the modern day Saffir–Simpson scale. The first system was initially observed in the northeastern Gulf of Mexico on June 26. The tenth and final system dissipated near Bermuda on November 10. These dates fall within the period with the most tropical cyclone activity in the Atlantic. In post-season analysis, two tropical cyclones that existed in October were added to HURDAT – the official Atlantic hurricane database. At one point during the season, September 3 through the following day, a set of three tropical cyclones existed simultaneously.
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