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A New England hurricane is a tropical cyclone originating in the Atlantic Ocean that affects the states of Connecticut, Rhode Island, Massachusetts, Vermont, New Hampshire, or Maine in the United States. Due to geography and climatology, the vast majority of tropical cyclone strikes to the New England region occur in Connecticut, Rhode Island, and eastern Massachusetts.
Since record keeping began for Atlantic tropical cyclones in 1851, there have been approximately 30 tropical cyclones to directly strike New England. [1] Due to the location of New England, most tropical cyclones that threaten the region tend to recurve out to sea, mainly due to upper-level steering patterns, such as the jet stream. Tropical cyclones also tend to weaken upon approach due to the cooler waters above 40 latitude (near southeastern Massachusetts). Thus, tropical cyclone formation near New England and over the Gulf of Maine is very unfavorable. However, tropical cyclones moving up the East Coast can rapidly approach the Connecticut and Rhode Island coast before the encounter the cooler waters off southeast Massachusetts, and strike far southern New England as a category 3 hurricane. Both Connecticut and Rhode Island have been struck several times by a major hurricane since 1850.
Most commonly, New England will see the remnants or weakening stage of most tropical cyclones that make landfall either along the United States east coast or Gulf coast. This can sometimes lead to excessive rainfall, and in some cases destructive flooding. Hurricane Diane in 1955 produced over 19 inches of rain in Massachusetts and contributed to the 1955 Connecticut floods, one of the worst flooding events in Connecticut's history. [2] More recently, in 2011, a weakening Hurricane Irene produced historic flooding in Vermont, causing over $175 million in damage. [3]
The return period for hurricane and major landfalls along the coast of New England is highest in Connecticut and Rhode Island, and declines rapidly north toward Maine. Generally, the return period for hurricane force winds is 12-16 years along the coast of Connecticut and Rhode Island (which is for example higher than the coast of Georgia much farther south), to more than 50 years along the Maine coast. [4]
Due to the fact that sea surface temperatures from eastern Massachusetts northward are generally too cool to support a major tropical cyclone, the region very rarely sees a major hurricane landfall (Category 3 or higher). Since 1851, only 3 major hurricanes have ever made landfall on the New England coastline, and all of these were in Connecticut and Rhode Island. The return period for storms of such strength along the southern New England coastline is considered to be 50-70 years, and upwards of 300 years in coastal Maine. [5] As of 2022, the most recent major hurricane to make landfall in the region was Hurricane Carol in 1954.
On September 21, 1938, a Category 3 hurricane made landfall over New Haven, Connecticut with sustained winds of 115 mph (gusts of 150 mph) and a pressure of 941 millibars. Many coastal towns and cities on the Connecticut and Rhode Island coast suffered extreme damage. The coastal community of Napatree Point, Rhode Island was hit with a 20 - foot storm surge and the day after the cyclone was totally gone (34 killed). The cyclone produced very high wind gusts inland at higher elevations, delivering a 186 mph wind gust to the Blue Hill Observatory in Massachusetts, a 163 mph gust atop Mount Washington. A storm surge of 10-18 feet from Long Island Sound to Narragansett Bay, it is often considered to be the most intense hurricane to ever strike New England in modern times. [6] One estimate from Rhode Island stated the water level "reflects a storm occurring roughly once every 400 years. A study of sand deposits also gives more evidence that this was the strongest hurricane to hit Rhode Island in over 300 years, since 1635." [7]
Saffir–Simpson scale | ||||||
TD | TS | C1 | C2 | C3 | C4 | C5 |
Multiple intense hurricanes (Category 3+) are noted to have possibly struck New England in pre-Columbian times: between 1100 and 1150, 1300–1400 (1295–1407), and 1400–1450 (1404–1446), respectively. [8] [9]
This article needs to be updated. The reason given is: At the very least, needs to mention Beryl and Debby, but possibly much more..(November 2024) |
A landfall in New England occurs only if the center of the storm comes ashore in Maine, New Hampshire, Massachusetts, Rhode Island, or Connecticut as they all share a coastline. Tropical cyclones that made landfall outside of New England, but subsequently passed through the region, are excluded from this category. For example, the 1893 New York hurricane, Tropical Storm Doria of 1971, and Hurricane Irene of 2011 all made landfall in New York City, but failed to cross Long Island Sound and enter Connecticut along its coastline. In addition, other systems such as the 1876 San Felipe hurricane, 1888 Louisiana hurricane, 1893 Sea Islands hurricane, and Hurricane Able of 1952 all passed through New York, to the north of New York City, before entering New England.
A landfall is also distinct from a direct hit, in which the eyewall, or core of the highest winds, comes onshore, without the center of the storm moving ashore. [79]
New England hurricanes have made landfall on many occasions. Normally, due to cold SSTs and high wind shear, hurricanes do not last long, so the ones that do make landfall are normally weak, with major hurricanes (Category 3 or higher) being rare. [80]
The following tables are a list of all tropical cyclones that have made landfall in New England since records began in 1851:
The 19th century saw a few notable storms. In 1869 an intense Category 3 hurricane struck Southeastern New England. Other hurricanes that made landfall include the Equinoctial Storm, Expedition hurricane, and the Saxby Gale. Since hurricanes were not named and fewer records were kept at the time, the information on some of the storms remains incomplete.
Name | Category | Season | Date of landfall | |
---|---|---|---|---|
Peak intensity | Intensity at landfall | |||
Unnamed | Tropical storm | Tropical storm | 1851 | October 19, 1851 |
Unnamed | Category 2 | Category 1 | 1858 | September 16, 1858 |
"Equinoctial" | Category 1 | Tropical storm | 1861 | September 28, 1861 |
"Expedition" | Category 1 | Tropical storm | 1861 | November 3, 1861 |
"Great September" | Category 3 | Category 3 | 1869 | September 8, 1869 |
"Saxby" | Category 2 | Category 2 | 1869 | October 4, 1869 |
Unnamed | Category 1 | Tropical storm | 1872 | October 27, 1872 |
Unnamed | Category 1 | Tropical storm | 1874 | September 30, 1874 |
Unnamed | Category 3 | Category 1 | 1879 | August 19, 1879 |
Unnamed | Category 1 | Category 1 | 1888 | September 26, 1888 |
Unnamed | Category 2 | Tropical storm | 1889 | September 25, 1889 |
Unnamed | Category 3 | Category 1 | 1894 | October 10, 1894 |
Unnamed | Category 3 | Category 1 | 1896 | September 10, 1896 |
Unnamed | Tropical storm | Tropical storm | 1897 | September 24, 1897 |
The 20th century saw eight hurricanes making landfall in New England; out of these the more notable include the 1938 New England hurricane (also called the Long Island Express), which made landfall as a major hurricane; [81] Hurricane Carol did the same sixteen years later. [82] The last hurricane to make landfall in New England was Hurricane Bob in 1991 as a Category 2 hurricane with maximum sustained winds of 100 mph. [83]
Name | Category | Season | Date of landfall | |
---|---|---|---|---|
Peak intensity | Intensity at landfall | |||
Unnamed | Category 1 | Tropical storm | 1908 | May 30, 1908 |
Unnamed | Category 2 | Tropical storm | 1916 | July 21, 1916 |
Unnamed | Tropical storm | Tropical storm | 1923 | October 19, 1923 |
Unnamed | Category 2 | Tropical storm | 1934 | September 9, 1934 |
"New England" | Category 5 | Category 3 | 1938 | September 21, 1938 |
"Great Atlantic" | Category 4 | Category 1 | 1944 | September 15, 1944 |
Carol | Category 3 | Category 3 | 1954 | August 31, 1954 |
Edna | Category 3 | Category 2 | 1954 | September 11, 1954 |
Cindy | Category 1 | Tropical storm | 1959 | July 11, 1959 |
Brenda | Tropical storm | Tropical storm | 1960 | July 30, 1960 |
Donna | Category 4 | Category 1 | 1960 | September 12, 1960 |
Tropical Storm Six | Tropical storm | Tropical storm | 1961 | September 15, 1961 |
Esther | Category 5 | Tropical storm | 1961 | September 26, 1961 |
Heidi | Tropical storm | Tropical storm | 1971 | September 14, 1971 |
Belle | Category 3 | Tropical storm | 1976 | August 10, 1976 |
Gloria | Category 4 | Category 1 | 1985 | September 27, 1985 |
Bob | Category 3 | Category 2 | 1991 | August 19, 1991 |
Bertha | Category 3 | Tropical storm | 1996 | July 13, 1996 |
Floyd | Category 4 | Tropical storm | 1999 | September 16–17, 1999 |
So far in the 21st century, five tropical cyclones have made landfall in New England: Tropical Storm Hermine in 2004, which made landfall in southeastern Massachusetts; Tropical Storm Beryl in 2006, which made landfall in Nantucket; Tropical Storm Hanna in 2008, which made landfall in Connecticut; and Tropical Storms Elsa and Henri in 2021, which both made landfall in Rhode Island.
Name | Category | Season | Date of landfall | |
---|---|---|---|---|
Peak intensity | Intensity at landfall | |||
Hermine | Tropical storm | Tropical storm | 2004 | August 31, 2004 |
Beryl | Tropical storm | Tropical storm | 2006 | July 21, 2006 |
Hanna | Category 1 | Tropical storm | 2008 | September 6, 2008 |
Elsa | Category 1 | Tropical storm | 2021 | July 9, 2021 |
Henri | Category 1 | Tropical storm | 2021 | August 22, 2021 |
Some tropical cyclones that have impacted New England have resulted in fatalities in the region. The most notorious and deadly of these storms is the 1938 New England hurricane which killed between 682 and 800 people. This list includes all tropical cyclones that have resulted in at least 10 deaths in New England. Some storms may be excluded or their death toll may be inaccurate due to a lack of available data at the time.
Name | Year | Number of deaths |
---|---|---|
"New England" | 1938 | 682-800 |
Unnamed | 1849 | 143 |
Unnamed | 1927 | 85 |
Unnamed | 1841 | 81 |
Carol | 1954 | 68 |
Unnamed | 1778 | 50-70 |
"Great Colonial" | 1635 | 46+ |
Unnamed | 1917 | 41 |
Unnamed | 1815 | 38+ |
"Great Atlantic" | 1944 | 28 |
Unnamed | 1878 | 27 |
Edna | 1954 | 21 |
"Snow" | 1804 | 16 |
Irene | 2011 | 16 |
"Great September" | 1869 | 12 |
Dog | 1950 | 12 |
Bob | 1991 | 12 |
Hurricane Gloria was a powerful hurricane that caused significant damage along the east coast of the United States and in Atlantic Canada during the 1985 Atlantic hurricane season. It was the first significant tropical cyclone to strike the northeastern United States since Hurricane Agnes in 1972 and the first major storm to affect New York City and Long Island directly since Hurricane Donna in 1960. Gloria was a Cape Verde hurricane originating from a tropical wave on September 16 in the eastern Atlantic Ocean. After remaining a weak tropical cyclone for several days, Gloria intensified into a hurricane on September 22 north of the Lesser Antilles. During that time, the storm had moved generally westward, although it turned to the northwest due to a weakening of the ridge. Gloria quickly intensified on September 24, and the next day reached peak winds of 145 mph (233 km/h). The hurricane weakened before striking the Outer Banks of North Carolina on September 27. Later that day, Gloria made two subsequent landfalls on Long Island and across the coastline of western Connecticut, before becoming extratropical on September 28 over New England. The remnants moved through Atlantic Canada and went on to impact Western Europe, eventually dissipating on October 4.
The 1954 Atlantic hurricane season was an above-average Atlantic hurricane season in terms of named storms, with 16 forming. Overall, the season resulted in $751.6 million in damage, the most of any season at the time. The season officially began on June 15, and nine days later the first named storm developed. Hurricane Alice developed in the Gulf of Mexico and moved inland along the Rio Grande, producing significant precipitation and record flooding that killed 55 people. Activity was slow until late August; only Barbara, a minimal tropical storm, developed in July. In the span of two weeks, hurricanes Carol and Edna followed similar paths before both striking New England as major hurricanes. The latter became the costliest hurricane in Maine's history.
Hurricane Carol was among the worst tropical cyclones on record to affect the states of Connecticut and Rhode Island in the United States. It developed from a tropical wave near the Bahamas on August 25, 1954, and slowly strengthened as it moved northwestward. On August 27, Carol intensified to reach winds of 105 mph (169 km/h), but weakened as its motion turned to a northwest drift. A strong trough of low pressure turned the hurricane northeastward, and Carol later intensified into a major hurricane. While paralleling the Mid-Atlantic and Southeastern United States, the storm produced strong winds and rough seas that caused minor coastal flooding and slight damage to houses in North Carolina, Virginia, Washington, D.C., Delaware, and New Jersey. The well-organized hurricane accelerated north-northeastward and made landfall on eastern Long Island, New York, and then over eastern Connecticut on August 31 with sustained winds estimated at 110-mph and a barometric pressure near 956 mb. Carol later transitioned into an extratropical cyclone over New Hampshire, on August 31, 1954.
Hurricane Edna was a deadly and destructive major hurricane that impacted the United States East Coast in September of the 1954 Atlantic hurricane season. It was one of two hurricanes to strike Massachusetts in that year, the other being Hurricane Carol. The fifth tropical cyclone and storm of the season, as well as the fourth hurricane and second major hurricane, Edna developed from a tropical wave on September 2. Moving towards the north-northwest, Edna skirted the northern Leeward Islands as a tropical depression before turning more towards the west. The depression attained tropical storm status to the east of Puerto Rico and strengthened further to reach hurricane status by September 7. The storm rapidly intensified and reached its peak intensity of 125 mph (205 km/h) north of the Bahamas before weakening to Category 2 status near landfall in Massachusetts on September 11. Edna transitioned into an extratropical cyclone in Atlantic Canada before its remnants dissipated in the northern Atlantic.
Hurricane Belle was a strong tropical cyclone that caused moderate damage across the East Coast of the United States in August 1976. In late July, a tropical wave emerged off the west coast of Africa. Traversing the Atlantic Ocean for more than a week, the system eventually consolidated into a tropical depression near the Bahamas on August 6. Remaining nearly stationary for a day, the depression strengthened into a tropical storm on August 7 and a hurricane later that day as it acquired a northwest motion. Formation of an eye accompanied quick intensification and Belle reached its peak the following day with winds of 120 mph (190 km/h). The hurricane subsequently turned north and accelerated, skirting the Outer Banks of North Carolina. Early on August 10, Belle made landfall on Long Island, New York, as a minimal hurricane crossing Long Island Sound and hitting the central coast of Connecticut as a strong tropical storm. Thereafter, Belle transitioned into an extratropical cyclone over New England before moving over Atlantic Canada. The system turned east while over the North Atlantic and ultimately dissipated on August 15 to the south of Iceland.
Hurricane Ginny was the strongest recorded tropical cyclone to make landfall in Canada at the time, until being eclipsed by Hurricane Fiona in 2022, as well as the latest hurricane on a calendar year to affect the U.S. state of Maine. The eighth tropical storm, as well as the seventh and final hurricane of the 1963 Atlantic hurricane season, Ginny developed on October 16 over the Bahamas, although it was not initially a fully tropical cyclone. As it moved to the North and later northwest, Ginny intensified to hurricane status as it became more tropical. For eight days, it was located within 250 mi (400 km) of the United States coastline. After approaching North Carolina, Ginny looped to the southwest and approached within 50 mi (80 km) of the Florida coastline. It turned to the North, to the East, and later to the northeast, strengthening late in its duration to peak winds of 110 mph (175 km/h). Ginny became an extratropical cyclone shortly after striking Nova Scotia at its peak intensity on October 29.
Hurricane Dog was the most intense hurricane in the 1950 Atlantic hurricane season. Prior to reanalysis by the Hurricane Research Division in 2014, it was considered one of the strongest Atlantic hurricanes on record, equivalent to Category 5 status on the modern Saffir-Simpson scale, with winds of 185 miles per hour (298 km/h). The fourth named storm of the season, Dog developed on August 30 to the east of Antigua; after passing through the northern Lesser Antilles, it turned to the north and intensified into a Category 4 hurricane. Dog reached its peak intensity with winds of 145 mph (230 km/h) over the open Atlantic, and after weakening it passed within 200 miles (320 km) of Cape Cod, Massachusetts. The storm became extratropical on September 12.
Hurricane Esther was the first large tropical cyclone to be discovered by satellite imagery. The fifth tropical cyclone, named storm, and hurricane of the 1961 Atlantic hurricane season, Esther developed from an area of disturbed weather hundreds of miles west-southwest of the southernmost Cape Verde Islands on September 10. Moving northwestward, the depression strengthened into Tropical Storm Esther on September 11, before reaching hurricane intensity on the following day. Early on September 13, Esther curved westward and deepened into a major hurricane. The storm remained a Category 3 hurricane for about four days and gradually moved in a west-northwestward direction. Late on September 17, Esther strengthened into a Category 5 hurricane with sustained winds of 160 mph (260 km/h) on September 18. The storm curved north-northeastward on September 19, while offshore of North Carolina. Esther began to weaken while approaching New England and fell to Category 3 intensity on September 21. The storm turned eastward early on the following day, and rapidly weakened to a tropical storm.
Hurricane Edouard was the strongest hurricane of the 1996 Atlantic hurricane season, reaching winds of 145 mph (233 km/h) on its path. Edouard remained a major hurricane for eight days, an unusually long amount of time. A Cape Verde hurricane, the storm formed near the coast of Africa in the middle of August. It moved westward then curved northward, and persisted until early September when it became extratropical to the southeast of New England. Edouard was originally forecast to strike the northeast United States, but it produced hurricane-force gusts to portions of southeastern Massachusetts while remaining offshore. The winds caused minor damage totaling $20 million. In addition, the hurricane generated strong waves and rip currents to coastlines, killing two people in Ocean City, New Jersey and causing numerous injuries.
Tropical Storm Josephine was an unusual Atlantic tropical storm that moved from west to east across the Gulf of Mexico in October 1996. It formed on October 4 as a tropical depression from the remnants of a cold front. Early in its duration, the system interacted with a ridge over the central United States, which produced strong winds and high tides along the Texas coast. The outer rainbands caused flooding rainfall in southern Texas, and in Louisiana, high tides flooded roads and stranded residents on Grand Isle. Moving generally to the east due to a trough, the depression intensified into a tropical storm on October 6, and the next day reached peak winds of 70 mph (110 km/h) while approaching the west coast of Florida. Josephine made landfall in Taylor County near peak intensity early on October 8, and soon after became extratropical. While moving ashore, the storm produced a high storm surge reaching 9.3 ft (2.8 m) in Suwannee. High tides flooded about 3,600 houses along the west coast. Josephine also produced heavy rainfall, which flooded hundreds of homes, and high winds, which left 400,000 people without power. The storm also spawned at least 16 tornadoes, one of which damaged 130 homes.
Tropical Storm Doria was the costliest tropical cyclone in the 1971 Atlantic hurricane season. The fifth tropical storm of the season, Doria developed from a tropical wave on August 20 to the east of the Lesser Antilles, and after five days without development it attained tropical storm status to the east of Florida. Doria turned to the north, and reached peak winds of 65 mph (105 km/h) as it was making landfall near Morehead City, North Carolina. It turned to the northeast, and moved through the Mid-Atlantic and New England as a tropical storm before becoming an extratropical storm over Maine on August 29.
Tropical Storm Carrie was a strong tropical storm that affected the East Coast of the United States in early September 1972. The third tropical cyclone of the 1972 Atlantic hurricane season, Carrie formed on August 29 from a complex sequence of meteorological events starting with the emergence of a tropical wave into the Atlantic in the middle of August.
The Christmas 1994 nor'easter was an intense cyclone along the East Coast of the United States and Atlantic Canada. It developed from an area of low pressure in the southeast Gulf of Mexico near the Florida Keys, and moved across the state of Florida. As it entered the warm waters of the Gulf Stream in the Atlantic Ocean, it began to rapidly intensify, exhibiting traits of a tropical system, including the formation of an eye. It attained a pressure of 970 millibars on December 23 and 24, and after moving northward, it came ashore near New York City on Christmas Eve. Because of the uncertain nature of the storm, the National Hurricane Center (NHC) did not classify it as a tropical cyclone.
Hurricane Gerda was a damaging Category 3 major hurricane which formed during the 1969 Atlantic hurricane season. It was the seventh named storm, fifth hurricane and third major hurricane of the 1969 season. Gerda formed on September 6 and crossed Florida as a tropical depression. Gerda later became a tropical storm after making a hard right turn and moving northeast and reaching hurricane status on September 8. Gerda brushed past the Outer Banks of North Carolina before reaching maximum intensity of 120 mph (190 km/h) and a low barometric pressure of 980 millibars (29 inHg). On September 10, Gerda made landfall near Eastport, Maine, and became extratropical the following day.
Hurricane Bob was one of the costliest hurricanes in New England history. The second named storm and first hurricane of the 1991 Atlantic hurricane season, Bob developed from an area of low pressure near The Bahamas on August 16. The depression steadily intensified, and became Tropical Storm Bob late on August 16. Bob curved north-northwestward as a tropical storm, but re-curved to the north-northeast after becoming a hurricane on August 17. As such, it brushed the Outer Banks of North Carolina on August 18 and August 19, and subsequently intensified into a major hurricane. After peaking in intensity with maximum sustained winds of 115 mph (185 km/h), Bob weakened slightly as it approached the coast of New England.
Tropical Storm Dean caused minor flooding along portions of the East Coast of the United States in September 1983. The seventh and final tropical cyclone of the very inactive 1983 Atlantic hurricane season, Dean developed from a frontal low to the northeast of the Bahamas on September 26. Initially subtropical, it gained characteristics of a tropical cyclone while tracking slowly north-northeastward. By September 27, the system was reclassified as Tropical Storm Dean. While tracking northward on September 28, Dean peaked with winds of 65 mph (100 km/h), shortly before curving west-northwestward and slowly leveling-off in intensity. Eventually, Dean made landfall in Virginia on the Delmarva Peninsula on September 29 as a weakening tropical storm. Dean rapidly weakened over land and was no longer classifiable as a tropical cyclone by early on October 1.
Hurricane How was the only tropical cyclone to make landfall on the United States in 1951. It was the eighth storm of the season, forming on September 28 in the northwest Caribbean and, after entering the Gulf of Mexico, turned eastward and became a tropical storm. The storm brought heavy rainfall to Florida, causing flooding and $2 million in damage. Tropical Storm How later became a hurricane, passing near the Outer Banks of North Carolina where it produced strong winds and high tides. A ship called the "Southern Isles" capsized off Cape Hatteras, killing 17 out of the crew of 23. Rains and high tides occurred in southeastern New England, before the hurricane moved out to sea and became extratropical.
The 1869 Atlantic hurricane season was the earliest season in the Atlantic hurricane database in which there were at least ten tropical cyclones. Initially there were only three known storms in the year, but additional research uncovered the additional storms. Meteorologist Christopher Landsea estimates up to six storms may remain missing from the official database for each season in this era, due to small tropical cyclone size, sparse ship reports, and relatively unpopulated coastlines. All activity occurred in a three-month period between the middle of August and early October.
The 1940 New England hurricane moved off of the U.S. East Coast and Atlantic Canada in August and September 1940, producing strong winds and torrential rainfall. The fourth tropical cyclone and third hurricane of the season, the storm originated from a well-defined low-pressure area in the open Atlantic Ocean on August 26. Moving slowly in a general west-northwest motion, the disturbance intensified, reaching tropical storm strength on August 28 and subsequently hurricane intensity on August 30. The hurricane passed within 85 mi (137 km) of Cape Hatteras before recurving towards the northeast. The hurricane continued to intensify, and reached peak intensity as a Category 2 hurricane with maximum sustained winds of 110 mph (180 km/h) and a minimum barometric pressure of 961 mbar, though these statistical peaks were achieved at different times on September 2. Afterwards, the hurricane began a weakening trend as it proceeded northeastward, and had degenerated into a tropical storm by the time it made its first landfall on Nova Scotia later that day. The storm transitioned into an extratropical cyclone the next day while making another landfall on New Brunswick. The extratropical remnants persisted into Quebec before merging with a larger extratropical system late on September 3.
Hurricane Arthur was the earliest known hurricane to make landfall in the U.S. state of North Carolina during the calendar year. It was also the first hurricane to make landfall in the United States since Hurricane Isaac in 2012. The first named storm of the 2014 Atlantic hurricane season, Arthur developed from an initially non-tropical area of low-pressure over the Southeastern United States that emerged into the western Atlantic Ocean on June 28. After sufficiently organizing, developing a well-defined circulation and deep convection amid a favorable environment, it was classified as a tropical depression on July 1. The system continued to strengthen and was declared a tropical storm later that day. Drifting northward, the storm reached hurricane status early on July 3 and curved toward the north-northeast. Further structural organization resulted in additional intensification, and by 01:00 UTC on July 4, the system attained its peak winds of 100 mph (160 km/h) as a Category 2 hurricane on the Saffir–Simpson hurricane wind scale. Arthur made landfall at 03:15 UTC over North Carolina's Shackleford Banks, positioned between Cape Lookout and Beaufort, and intensified slightly further, with a minimum atmospheric pressure of 973 mbar. The storm then trekked swiftly northeast, weakening as it passed by Cape Cod and Nantucket, before transitioning into an extratropical cyclone and coming ashore at Weymouth, Nova Scotia, on July 5. The remnants continued generally northeastward through Atlantic Canada before ultimately dissipating on July 9 over the Labrador Sea.
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