1938 New England hurricane
|Category 5 major hurricane (SSHWS/NWS)|
|Formed||September 9, 1938|
|Dissipated||September 23, 1938|
|(Extratropical after September 22)|
1-minute sustained: 160 mph (260 km/h) |
|Lowest pressure||< 940 mbar (hPa); 27.76 inHg|
|Fatalities||682 to 800 direct|
|Damage||$306 million (1938 USD)|
|Areas affected||Southeastern United States, Northeastern United States (particularly Connecticut, New York, Rhode Island, and Massachusetts), southwestern Quebec|
|Part of the 1938 Atlantic hurricane season|
The 1938 New England Hurricane (also referred to as the Great New England Hurricane, Long Island Express, and Yankee Clipper) was one of the deadliest and most destructive tropical cyclones to strike Long Island, New York and New England. The storm formed near the coast of Africa on September 9, becoming a Category 5 hurricane on the Saffir-Simpson Hurricane Scale before making landfall as a Category 3 hurricane on Long Island on September 21. It is estimated that the hurricane killed 682 people, damaged or destroyed more than 57,000 homes, and caused property losses estimated at $306 million ($4.7 billion in 2016). Damaged trees and buildings were still seen in the affected areas as late as 1951. It remains the most powerful and deadliest hurricane in recorded New England history, perhaps eclipsed in landfall intensity only by the Great Colonial Hurricane of 1635.
- 1 Meteorological history
- 2 Forecasting the storm
- 3 Impact
- 4 See also
- 5 References
- 6 Further reading
- 7 Bibliography
- 8 External links
The storm was first analyzed by ship data south of the Cape Verde Islands on September 9. Over the next 10 days, it steadily gathered strength and slowly tracked to the west-northwest; it is estimated to have reached Category 5 intensity by September 20, while centered east of the Bahamas. It then veered northward in response to a deep trough over Appalachia, sparing the Bahamas, Florida, the Carolinas, and the Mid-Atlantic states. At the same time, a high pressure system was centered north of Bermuda, preventing the hurricane from making an eastward turn out to sea.
Thus, the hurricane was effectively squeezed to the north between the two weather systems. This caused the storm's forward speed to increase substantially late on September 20. This extreme forward motion was in the same general direction as the winds on the eastern side of the storm as it proceeded north; this, in turn, caused the wind speed to be far higher in areas east of the storm's eye than would be the case with a hurricane of more typical forward speed.
The storm was centered several hundred miles to the southeast of Cape Hatteras during the early hours of September 21, and it weakened slightly. By 8:30 am EDT, it was centered approximately 100 miles (160 km) due east of Cape Hatteras, and its forward speed had increased to well over 50 mph. This rapid movement did not permit enough time for the storm to weaken over the cooler waters before it reached Long Island. The hurricane sped through the Virginia tidewater during the 9:00 am hour. Between 12:00 pm and 2:00 pm, the New Jersey coastline and New York City caught the western edge. At the same time, weather conditions began to deteriorate rapidly on Long Island and along the southern New England coast.
The hurricane made landfall at Bellport on Long Island's Suffolk County sometime between 2:10 pm and 2:40 pm as a Category 3 hurricane, with sustained winds of 120 mph. It made a second landfall as a Category 3 hurricane somewhere between Bridgeport and New Haven, Connecticut at around 4:00 pm, with sustained winds of 115 mph.
The storm's eye moved into western Massachusetts by 5:00 pm, and it reached Vermont by 6:00 pm. Both Westfield, Massachusetts and Dorset, Vermont reported calm conditions and partial clearing during passage of the eye, which is a rather unusual occurrence for a New England hurricane. The hurricane began to lose tropical characteristics as it continued into northern Vermont, though it was still carrying hurricane-force winds. It crossed into Quebec at approximately 10:00 pm, transitioning into a post-tropical low. The post-tropical remnants dissipated over northern Ontario a few days later.
Forecasting the storm
In 1938, United States forecasting lagged behind forecasting in Europe, where new techniques were being used to analyze air masses, taking into account the influence of fronts. A confidential report was released by the United States Forest Service, the parent agency of the United States Weather Bureau. It described the weather bureau's forecasting as "a sorry state of affairs" where forecasters had poor training and systematic planning was not used, and where forecasters had to "scrape by" to get information wherever they could. The Jacksonville, Florida, office of the weather bureau issued a warning on September 19 that a hurricane might hit Florida. Residents and authorities made extensive preparations, as they had endured the Labor Day Hurricane three years earlier. When the storm turned north, the office issued warnings for the Carolina coast and transferred authority to the bureau's headquarters in Washington.
At 9:00 am on September 21, the Washington office issued northeast storm warnings north of Atlantic City and south of Block Island, Rhode Island, and southeast storm warnings from Block Island to Eastport, Maine. The advisory, however, underestimated the storm's intensity and said that it was farther south than it actually was. The office had yet to forward any information about the hurricane to the New York City office. At 10:00 am, the bureau downgraded the hurricane to a tropical storm. The 11:30 am advisory mentioned gale-force winds but nothing about a tropical storm or hurricane.
That day, 28 year-old rookie Charles Pierce was standing in for two veteran meteorologists. He concluded that the storm would be squeezed between a high-pressure area located to the west and a high-pressure area to the east, and that it would be forced to ride up a trough of low pressure into New England. A noon meeting was called and Pierce presented his conclusion, but he was overruled by "celebrated" chief forecaster Charles Mitchell and his senior staff. In Boston, meteorologist E.B. Rideout told his WEEI radio listeners (to the skepticism of his peers) that the hurricane would hit New England. At 2:00 pm, hurricane-force gusts were occurring on Long Island's South Shore and near hurricane-force gusts on the coast of Connecticut. The Washington office issued an advisory saying that the storm was 75 miles east-southeast of Atlantic City and would pass over Long Island and Connecticut. Re-analysis of the storm suggests that the hurricane was farther north (just 50 miles from Fire Island), and that it was stronger and larger than the advisory said.
The majority of the storm damage was from storm surge and wind. Damage was estimated at $308 million, the equivalent of $5.1 billion adjusted for inflation in 2016 dollars, making it among the most costly hurricanes to strike the U.S. mainland. It is estimated that, if an identical hurricane had struck in 2005, it would have caused $39.2 billion in damage due to changes in population and infrastructure.
In total, 4,500 cottages, farms, and other homes were reported destroyed and 25,000 homes were damaged. Other damages included 26,000 automobiles destroyed and 20,000 electrical poles toppled. The hurricane also devastated the forests of the Northeast, knocking down an estimated two billion trees in New York and New England. Freshwater flooding was minimal, however, as the quick passage of the storm decreased local rainfall totals, with only a few small areas receiving over 10 inches (250 mm).
Over 35% of New England's total forest area was affected. In all, over 2.7 billion board feet of trees fell because of the storm, although 1.6 billion board feet of the trees were salvaged. The Northeastern Timber Salvage Administration (NETSA) was established to deal with the extreme fire hazard that the fallen timber had created. In many locations, roads from the fallen tree removal were visible decades later, and some became trails still used today. The New York, New Haven and Hartford Railroad from New Haven to Providence was particularly hard hit, as countless bridges along the Shore Line were destroyed or flooded, severing rail connections to badly affected cities such as Westerly, Rhode Island.
Due to the lack of technology in 1938, Long Island residents were not warned of the hurricane's arrival, leaving no time to prepare or evacuate. Long Island was struck first, before New England and Quebec, earning the storm the nickname the "Long Island Express." The winds reached up to 150 mph with waves surging to around 25–35 feet high.
Yale and Harvard both owned large forests managed by their forestry departments, but both forests were wiped out by the hurricane. However, Yale had a backup forest at Great Mountain in northwestern Connecticut which was spared from the totality of the damages, and they were able to keep their forestry program running, which maintains operation today. Harvard's program, however, was reduced as a result.
The western side of the hurricane caused sustained tropical storm-force winds, high waves, and storm surge along the Jersey Shore and destroyed much of the boardwalk in Atlantic City. The Brigantine Bridge was destroyed over Absecon Inlet between Atlantic City and Brigantine, New Jersey. The surge inundated several coastal communities; Wildwood was under 3 feet (0.91 m) of water at the height of the storm, and the boardwalk was destroyed in Bay Head and dozens of cottages washed into the ocean. Crops sustained wind damage. The maximum recorded wind gust was 70 mph at Sandy Hook.
New York City and western Long Island
The metropolitan area escaped the worst of the wind and storm surge because it was hit by the storm's weaker western side. Winds were recorded at 60 mph at Central Park, Battery Park recorded sustained winds of 70 mph with gusts to 80 mph, and a gust of 90 mph was recorded 500 feet above ground at the Daily News Building. Winds were estimated at 120 mph on top of the Empire State Building. The highest winds were from the north to northwest on the back side of the storm. The storm surge was 8½ feet at the Battery and the Mean Low Water storm tide was 16¾ feet at Willets Point. In New York Harbor, the waters rose 7 feet in a half-hour.
In New York City and Long Island, schools were dismissed early. Extensive street flooding occurred because debris blocked drains. The East River flowed three blocks and flooded a Consolidated Edison (Con Ed) plant at 133rd Street, causing power to fail in Manhattan north of 59th Street and in the Bronx for several minutes to a few hours. Railroad and ferry services were suspended for a time. The Staten Island Ferry boat Knickerbocker got stuck in the terminal with 200 passengers aboard. Bridges and tunnels into Manhattan were closed until the following afternoon. 95% of Nassau County lost power, where floods brought traffic to a halt.
In Manhasset Bay, almost 400 boats were ripped from their moorings and smashed or sunk, with more than 100 washing up on the beach by the Port Washington Yacht Club. Similar scenes occurred in other locations on the north shore. The J.P. Morgan estate in Glen Cove was heavily damaged. The wife of New York City mayor Fiorello La Guardia was forced to wait out the storm on the second floor of their Northport cottage. Mitchel Field army airfield was buffeted by winds of nearly 100 mph and was under knee-deep water. In Williston Park, residents of 50 homes needed to be rescued by rowboat when heavy rain the previous few days combined with the rain from the hurricane to overflow a pond.
Eastern Long Island
Eastern Long Island experienced the worst of the storm. The Dune Road area of Westhampton Beach was obliterated, resulting in 29 deaths. There were 21 other deaths through the rest of the east end of Long Island. The storm surge temporarily turned Montauk into an island as it flooded across the South Fork at Napeague and obliterated the tracks of the Long Island Rail Road.
Long Island was hit hard being exposed to the storm due to its shorelines. The estimated storm tide was 15 feet in this region. A mean low water storm tide of 8 feet was recorded at Port Jefferson. About 50 people perished in the storm's wake. All the shore lines were very vulnerable to the high winds and flooding, and anyone near the shores was directly in harm's way.
Ten new inlets were created on eastern Long Island. The surge rearranged the sand at the Cedar Point Lighthouse so that the island became connected to what is now Cedar Point County Park. The surging water created the Shinnecock Inlet by carving out a large section of barrier island separating Shinnecock Bay from the Atlantic. The storm toppled the landmark steeple of the Old Whaler's Church, which was the tallest building in Sag Harbor. The steeple has not been rebuilt.
Wading River suffered substantial damage. The storm blew down the movie theater on Front Street in Greenport on the North Fork of Long Island. The fishing industry was destroyed, as was half of the apple crop.
The storm surge hit Westerly, Rhode Island at 3:50 pm, resulting in 100 deaths. The tide was higher than usual because of the autumnal equinox and full moon, and the hurricane produced storm tides of 14 to 18 feet (5 m) along most of the Connecticut coast, with 18 to 25-foot (8 m) tides from New London east to Cape Cod—including the entire coastline of Rhode Island.
The storm surge was especially violent along the Rhode Island shore, sweeping hundreds of summer cottages out to sea. Low-lying Block Island was almost completely underwater, and many drowned. As the surge drove northward through Narragansett Bay, it was restricted by the Bay's funnel shape and rose to 15.8 feet above normal spring tides, resulting in more than 13 feet (4.0 m) of water in some areas of downtown Providence. Several motorists were drowned in their automobiles. In Jamestown, seven children were killed when their school bus was blown into Mackerel Cove. Many stores in downtown Providence were looted by mobs, often before the flood waters had fully subsided and due in part to the economic difficulties of the Great Depression.
Many homes and structures were destroyed along the coast, as well as many structures inland along the hurricane's path. Entire beach communities were obliterated on the coast of Rhode Island. Napatree Point was completely swept away, a small cape that housed nearly 40 families between the Atlantic Ocean and Little Narragansett Bay just off of Watch Hill. Today, Napatree is a wildlife refuge with no human inhabitants. One house in Charlestown, Rhode Island was lifted and deposited across the street, where it stood until it was demolished in August 2011. Even to this day, concrete staircases and boardwalk bases destroyed by the hurricane can be found when sand levels are low on some beaches. The boardwalk along Easton's Beach in Newport was completely destroyed by the storm.
A few miles from Conanicut Island, Whale Rock Light was swept off its base and into the raging waves, killing lighthouse keeper Walter Eberle. His body was never found. The Prudence Island Light suffered a direct blow from the storm surge, which measured 17 feet 5 inches at Sandy Point. The masonry tower was slightly damaged. However, the adjoining light keeper's home was utterly destroyed and washed out to sea. The light keeper's wife and son were both killed, as well as the former light keeper and a couple who left their summer cottages near the lighthouse and sought shelter in what they thought was the sturdier light keeper's home. Light keeper George T. Gustavus was thrown free from the wreckage of the house and was saved by an island resident who held a branch into the water from the cliffs farther down the coast. Gustavus and Milton Chase, the owner of the island's power plant, reactivated the light during the storm by running a cable from the plant to the light and installing a light bulb, marking the first time that it was illuminated with electricity.
The original parchment of the 1764 Charter of Brown University was washed clean of its text when its vault was flooded in a Providence bank. Newport recorded the highest water level of the storm, at 3.53 meters above mean sea level according to a NOAA study. This storm level is 0.98 meters above the SLOSH model of a 100-year storm, and one estimate is that this water level "reflects a storm occurring roughly once every 400 years." A study of sand deposits also gives evidence that this was the strongest hurricane to hit Rhode Island in over 300 years. The Fox Point Hurricane Barrier was completed in 1966 because of the massive flooding from the 1938 storm, and from the even higher 14.4 foot (4.4 meters) storm surge that resulted from 1954's Hurricane Carol, in hopes of preventing extreme storm surges from ever again flooding downtown Providence.
Eastern Connecticut was on the eastern side of the hurricane. Long Island acted as a buffer against large ocean surges, but the waters of Long Island Sound rose to great heights. Small shoreline towns to the east of New Haven experienced much destruction from the water and winds, and the 1938 hurricane holds the record for the worst natural disaster in Connecticut's 350-year history. The mean low-water storm tide was 14.1 feet at Stamford, 12.8 feet at Bridgeport, and 10.58 feet at New London, which remains a record high.
In the shoreline towns of Madison, Clinton, Westbrook, and Old Saybrook, buildings were found as wreckage across coastal roads. Actress Katharine Hepburn waded to safety from her Old Saybrook beach home, narrowly escaping death. She stated in her 1991 book that 95% of her personal belongings were either lost or destroyed, including her 1932 Oscar, which was later found intact. In Old Lyme, beach cottages were flattened or swept away. The NYNH&H passenger train Bostonian became stuck in debris at Stonington. Two passengers drowned while attempting to escape before the crew was able to clear the debris and get the train moving. Along the Stonington shorefront, buildings were swept off their foundations and found two miles (3 km) inland. Rescuers found live fish and crabs in kitchen drawers and cabinets while searching for survivors in the homes in Mystic.
New London was first swept by the winds and storm surge, after which the waterfront business district caught fire and burned out of control for 10 hours. Stately homes along Ocean Beach were leveled by the storm surge. The permanently anchored 240-ton lightship at the head of New London Harbor was found on a sand bar two miles (3 km) away.
Interior sections of the state experienced widespread flooding as the hurricane's torrential rains fell on soil already saturated from previous storms. The Connecticut River was forced out of its banks, inundating cities and towns from Hartford to Middletown. Novelist Ann Petry drew on her personal experiences of the hurricane in Old Saybrook in her 1947 novel Country Place. The novel is set in the immediate aftermath of World War II, but Petry identified the 1938 storm as the source for the storm that is at the center of her narrative.
The eye of the storm followed the Connecticut River north into Massachusetts, where the winds and flooding killed 99 people. In Springfield, the river rose six to 10 feet (3 m) above flood stage, causing significant damage. Up to six inches (152 mm) of rain fell across western Massachusetts, which combined with over four inches (102 mm) that had fallen a few days earlier to produce widespread flooding. Flash flooding on the Chicopee River washed away the Chicopee Falls Bridge, while the Connecticut River flooded most of the Willimansett section. Residents of Ware were stranded for days and relied on air-dropped food and medicine. After the flood receded, the town's Main Street was a chasm in which sewer pipes could be seen.
To the east, the surge left Falmouth and New Bedford under eight feet of water. Two-thirds of the boats sank in New Bedford harbor. Several homes washed away on Atlantic Boulevard in Fall River, whose foundations can still be found on the beach today. The Blue Hill Observatory registered sustained winds of 121 mph (195 km/h) and a peak gust of 186 mph (299 km/h), which is the strongest hurricane-related surface wind gust ever recorded in the United States. A 50-foot wave, the tallest of the storm, was recorded at Gloucester.
The storm entered Vermont as a Category 1 hurricane at approximately 6:00 pm EDT, reaching northern Vermont, Burlington, and Lake Champlain around 8:00 pm. Hurricane-force winds caused extensive damage to trees, buildings, and power lines. Over 2,000 miles (3,200 km) of public roads were blocked, and it took months for crews to reopen some of the roads. In Montpelier, 120 miles (190 km) from the nearest coast, salt spray was seen on windows. A train was derailed in Castleton. The storm killed five people in Vermont. Maple and sugar groves were damaged. The 1938 hurricane has been the only tropical cyclone to make a direct hit on Vermont in its recorded history; it remains the only one known to have struck Vermont as a hurricane.
Even though the storm center tracked further west, through Vermont, New Hampshire received appreciable damage. As in Vermont, very high winds brought down numerous trees and electric lines, but rainfall totals in New Hampshire were significantly less than those in other states. Only 1 inch (25 mm) of rain fell in Concord. Damage at Peterborough was worse, however; total damage there was stated to be $500,000 (1938 dollars, $6.5 million in 2005), which included the destruction of 10 bridges. Much of the lower downtown burned because floodwaters prevented firefighters from reaching and extinguishing the blaze. Other communities also suffered considerable damage to forest resources. In New Hampshire, 13 people perished. At Mt. Washington, winds gusted to 163 miles per hour (262 km/h) and knocked down part of a trestle on the Cog Railway.
Maryland and Delaware
The western periphery of the hurricane brought heavy rain and gusty winds to Delaware and southeastern Maryland. Damage, if any, is believed to have been minimal.
As the hurricane was transitioning into an extratropical cyclone, it tracked into southern Quebec. By the time the system initially crossed into Canada, it continued to produce heavy rain and very strong winds, but interaction with land had taken its toll. Nevertheless, the hurricane managed to blow down numerous trees throughout the region. Otherwise, damage was generally minimal.
- List of Atlantic hurricanes
- List of Category 5 Atlantic hurricanes
- List of New England hurricanes
- List of wettest tropical cyclones in Massachusetts
- List of Delaware hurricanes
- Hurricane Sandy
- "The Great Hurricane of 1938 - The Long Island Express". Retrieved February 9, 2017.
- Scotti, R. A. "Sudden Sea — The Great Hurricane of 1938". Boston: Little, Brown & Co., 2003. Archived from the original on January 2, 2007. Retrieved November 30, 2007.
- "The Great Hurricane of 1938". The Boston Globe. July 19, 2005. Retrieved November 30, 2007.
- Lane, F.W. The Elements Rage (David & Charles 1966, ISBN ), p. 16.
- Lefebvre, Paul (October 19, 2016). "How a hurricane changed New England's forests". The Chronicle. Barton, Vermont. pp. 1B.
- Christine Gibson Archived December 5, 2010, at the Wayback Machine. "Our 10 Greatest Natural Disasters," American Heritage, Aug./Sept. 2006.
- Winds rotate counter-clockwise around all low pressure systems in the Northern Hemisphere. Winds on the right side of a hurricane (relative to the direction of the storm itself) are moving in the same general direction as the hurricane. Therefore, the forward motion increases the observed wind speed for points to the right of the eye of the hurricane and decreases the observed wind speed for points to the left of the eye. This occurs in a complex way that defies crude addition or subtraction of the forward motion from the intrinsic wind speed of the hurricane.
- NOAA website: THE GREAT NEW ENGLAND HURRICANE of 1938.
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- Goudsouzian p11,12,57
- Hurricanes in History at the United States National Hurricane Center.
- Ranked Using 2005 Inflation, Population, and Wealth Normalization.
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- The Great Hurricane of 1938 | Peeling Back the Bark. Retrieved August 20, 2013.
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- Daily Discussion and Climate Summary — Tuesday, September 21, 2010 – ANNIVERSARY OF GREAT NEW ENGLAND HURRICANE OF 1938 from the Blue Hill Observatory, Milton, Massachusetts Retrieved August 20, 2013.
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- Aviles, Lourdes B. Taken by Storm, 1938: A Social and Meteorological History of the Great New England Hurricane (2012)
- * Bergman, Jonathan C. "A New Deal for Disaster: The 'Hurricane of 1938' and Federal Disaster Relief Operations, Suffolk County, New York," Long Island Historical Journal (Sept 2007), 20#1 pp 15–39, shows how Federal relief efforts led to the modern disaster-response system
- Burns, Cherie (2005). The Great Hurricane: 1938. New York: Atlantic Monthly Press. ISBN 0-87113-893-X.
- Goudsouzian, Aram. "'What Do You Do With A Disaster?' Providence and the Hurricane of 1938," Rhode Island History (Sept 2004) 62#2 pp 26–48.
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- Scotti, R. A. (2003). Sudden Sea: The Great Hurricane of 1938. Boston: Little & Brown. ISBN 0-316-73911-1.
- Goudsouzian, Aram. New England Remembers The Hurricane of 1938. Memoirs Unlimited Inc, 2004. ISBN 978 1-8898-33-75-0.
Media related to New England Hurricane of 1938 at Wikimedia Commons
- The Hurricane of '38 — An American Experience Documentary
- Damage from the hurricane
- National Hurricane Center, Brian R. Jarvinen Storm Tides in 12 Tropical Cyclones (including four intense New England hurricanes).
- State University of New York: Suffolk County Community College – History of Storm
(San Felipe Segundo)
(Tied with 1926 Great Miami)
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