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But that was The Day After........
1938 Hurricane - September 21, 1938. WINDS: 120-mph (moving at 50-mph). PRESSU 27.94 inches/946 mb. STORM - SURGE: 12 - 16 feet above Mean Tide ? LEFT: Wind gusts well over 100-mph bring down the steeple of the oldest church in Danielson, Connecticut, during the 1938 Hurricane. RIGHT: Oceanfront home on Misquamicut Beach in Rhode Island after the 1938 Hurricane (Photos Courtesy of Providence Journal - 1940). * The 1938 Hurricane is the strongest tropical cyclone to strike the Atlantic coast between Virginia and Massachusetts since at least 1869. Along the Atlantic coast of the United States (north of Florida) - only Hurricanes Hugo (1989) and Hazel (1954) were more intense at landfall. Every record for wind speed, tidal surge, and barometric pressure in New York, Connecticut, and Rhode Island - can be traced to this single event. In terms of fatalities and property damage - the 1938 hurricane stands as one of the worst disasters in American history. In a matter of hours, 600 people were killed, 3500 were injured, and more than 75,000 buildings were damaged. The states of New York, Connecticut, and Rhode Island, suffered their worst natural disaster in recorded history. The tidal wave like storm-surge that hit Long Island and Rhode Island was so severe, that earthquake instruments 3,000-miles away recorded it on seismographs. As a final cruelty - the residents of the northeast had little or no warning that this extreme meteorological event was unfolding before them. The 1938 hurricane originated in the far eastern Atlantic. Reports from mariners place the storm 350 miles north of Puerto Rico on September 16th, then heading in the general direction of the Bahamas and Florida. However, by September 20th, the U.S. Weather Bureau received ship reports that the cyclone had now turned north - traveling roughly parallel to the U.S. coastline. This was a common motion for Atlantic hurricanes.* Thinking the storm would follow the normal northeast path and recurve out to sea east of Cape Hatteras, the Weather Service no longer considered the storm a threat. From later research and analysis, it appears the storm not only strengthened off the coastline of the southeastern United States, but rapidly accelerated northward. Instead of recurving out to sea - the storm headed straight north, hitting central Long Island, NY, then crossing the Connecticut coast near New Haven at 3:30 PM on Wednesday, September 21, 1938. The track of the 1938 hurricane from the tropical Atlantic to landfall in the Northeastern United States ( Track chart courtesy of National Hurricane Center). METEOROLOGICAL CONDITIONS At the time of landfall on central Long Island, sustained winds in the 1938 hurricane have been estimated at 115 to 120-mph. However, the extreme forward speed of the storm (estimated at up to 50-mph) increased the winds on the right side of the storm to much stronger values. Some conservative estimates place the peak winds to the east of the center at 150-mph along the immediate coastline. The strongest winds in the 38 cyclone occurred on eastern Long Island, in southeastern Connecticut, and in southern Rhode Island. However, because of the rapid movement of the storm - inland areas of eastern Massachusetts experienced sustained hurricane force winds as well. Few weather recording stations were located near the area of maximum winds - and an even lesser number survived the storm (Simpson & Riehl -1981). A gust of 120-mph was recorded at the Watch Hill Lighthouse in Rhode Island, before the weather tower collapsed. The Harbormaster's Office in New London, Connecticut, recorded sustained winds of 98-mph until the roof blew off. At Blue Hills Observatory south of Boston, winds of 121-mph with gusts to 186-mph were recorded. The Blue Hill measurements were taken at an elevation of 700 feet - significantly higher than the standard 33-foot elevation for wind measurements. However, Blue Hill, Massachusetts is more than 100-miles inland from where the 38 Hurricane made landfall. It seems likely that peak wind gusts on eastern Long Island, and along the Rhode Island coast were close to 150-mph. The true value of the peak winds in the 38 hurricane may never been known. The lowest barometric pressure recorded on land was 27.94 inches (946 mb) at the Coast Guard Station in Bellport, Long Island. In Connecticut, a low pressure of 27.99 inches (948 mb) was recorded on the Wesleyan campus in Middletown, while the Yale School of Forestry in New Haven, recorded a pressure of 28.05 inches (950 mb) on a barograph (Riehl-1981). Based on pressure reports, the eye of the 38 Hurricane was about 20 to 30-miles wide. On Long Island the eye passed over the area from Bellport to Southhampton. In Connecticut the eye crossed the coast from New Haven to Saybrook. The 1938 hurricane produced the some of the most extreme coastal flooding ever known on the United States Atlantic coast. The 38 storm created a very fast moving storm surge more characteristic of a strong category 4 hurricane (winds 131 - 155 mph). This occurred because of the combination of a strong hurricane, moving at an extreme forward speed (50-mph), and striking the coast at almost the exact time of the autumnal high tide. Tidal surges up to 16-feet above mean sea level on Long Island and Rhode Island, and up to 12-feet above m.s.l. in eastern Connecticut, have been estimated. Several newspaper reports from the time of the 38 hurricane report damage to buildings more than 20-feet above sea level. __________________________________________________ ______________________________________________ THE IMPACT The 1938 hurricane produced winds of unimaginable fury across eastern Long Island, eastern Connecticut, and southern Rhode Island. The power of the wind carried away roofs, church steeples, factory buildings, and thousands of smaller structures. On Long Island, several 300-foot steel and concrete-bolted RCA radio towers were twisted into unrecognizable shapes by the wind. In Stonington, Connecticut, the entire top floor of the three-story, 500,000 square-foot brick Schneider factory blew away. Many who experienced the 38 storm along the immediate coastline, reported the sound of the wind reached an incredible high pitch - almost a scream. The air became intensely humid. The sight and sounds of the storm even inspired a book - A Wind To Shake The World, by Everett S. Allen. The extreme storm surge of the 1938 hurricane was beyond anything coastal residents along the northeast coast had ever experienced or written about. There was no historical comparison. Several survivors along the coast of Rhode Island, stated that at the height of the hurricane, they saw a 40-foot fog bank rolling toward the beach, when the bank got closer, they realized it wasn't fog - it was water (Whipple - 1940). Along the open ocean facing coastal roads in Rhode Island and Long Island - the damage was horrific. Whole beach communities were swept away - some without a trace. Napatree Point, Rhode Island - before and after the Hurricane of 38. The 38 storm was a textbook example of what a severe tropical cyclone can do to a barrier island in a few hours. Two short docks are visible in the center of both photographs. (Photos Lewis R. Greene 1938). * At 3:50 P.M. on Napatree Point in Watch Hill, Rhode Island, the storm surge struck the two mile long barrier island with full fury. Forty-four summer homes, the yacht club building, and seventeen people were swept into the Atlantic and never seen again. In Westerly, the four mile long Misquamicut Beach was totally wiped clean of buildings, more than 500 beach homes were swept away. At least 100 people were killed in the Westerly area alone. Dozens of people, including whole families, clung to rooftops and floating debris, as they rode the wreckage across the bay to the mainland. In Charlestown, Green Hill, Matunuck, Jerusalem, Galilee, the story was the same- many were dead or missing. The 38 hurricane also sent a tidal surge of epic proportions funneling up Narragansett Bay. The bay shore towns of East Greenwich, Barrington, and Warwick suffered catastrophic damage. Whole rows of buildings collapsed into the raging surf. On Conanicut Island in the middle of Narraganset Bay, a school bus full of grade school children was swept off a narrow causeway and into the raging storm surge, killing seven of ten children. Providence was flooded with 14 feet of water, submerging hundreds of cars, trolleys, and buildings.*Hundreds of people were marooned on the upper floors of office buildings in downtown Providence. The one-hundred-seventeen year old, 71-foot steel-reinforced lighthouse tower on Whale Rock, could not even stand against the 38 hurricane - it was swept away, taking the lighthouse keeper to his death. As the 1938 hurricane engulfed Rhode Island all sense of normalcy and order were lost. The best and worst of human nature came out. As writer David Cornel De Jong looked out his third floor office at civilization slowly unraveling in downtown Providence he wrote: "They came, neck deep, or swimming, rising out of the water and disappearing through the demolished store windows. At first there were few, then there were hordes, assisting each other. They seemed organized, almost regimented, as if they'd daily drilled and prepared for this event, the like of which hadn't happened in a hundred and twenty years. They were brazen and insatiable; they swarmed like rats; they took everything. When a few policeman came past in a rowboat, they didn't stop their looting. They knew they outnumbered the police. " * LEFT: At 4:45 p.m. the storm surge of the 1938 hurricane reaches the very heart of Providence, Rhode Island. Waves can be seen in front of the Biltmore Hotel (right building), while marooned pedestrians gather on the steps of Providence City Hall. RIGHT: Looking down Dorrance Street at the height of the hurricane. (Photos Providence Journal 1940). * In the days following the cyclone southern Rhode Islanders were in a state of grief-stricken shock. The first days after the storm were a somber time - the dead and injured were everywhere. As police and fire rescue teams picked their way through the devastated coastal communities, the number of dead mounted quickly. In the first three days after the cyclone -132 bodies were recovered along the Rhode Island coastline. After five days - the number of known dead passed 200. Entire families had perished in the tidal surge. A week after the storm, more than 150 people were still missing. The number of dead mounted so fast - that morgues in the coastal towns of Rhode Island had to have embalming fluid sent from Providence (Allen - 1976). The scene was similar on eastern Long Island, New York. Although eastern Long Island was mostly rural in 1938, there were several small communities spread along the south shore. The combination of 150-mph wind gusts and a huge tidal surge - swept away all traces of civilization. The area from eastern Fire Island to Southhampton looked as if a 50-foot tidal wave had hit - nothing was left standing. The storm surge swept completely across the narrow island into the Bay. Most of the buildings on Fire Island and Westhampton Beach washed up on the mainland. The storm surge was of such fury, that it created a new inlet along the coast - Shinnecock Inlet. Around the Westhampton Beach area, Red Cross workers had to use utility grid maps to figure out where roads had been (Whipple 1969). More than 60 people were killed on eastern Long Island. Several of the dead were found wearing only shoes and socks - the wind had stripped all clothing. The eastern end of Fire Island, NY near Moriches Inlet after the 1938 hurricane. The main road through the island is just visible in the center of the lower portion of the photograph. More than 200 homes had been perched on dunes 20 feet high. The horrific storm tide swept nearly everything away. (Photo Courtesy Mitchel Field, 2nd Air Base Squadron - U.S. Army, NY 1938). * LEFT: Temporary morgue on eastern Long Island following the 38 hurricane. RIGHT: Buildings in a tidal marsh near Newport, Rhode Island after the storm (Courtesy Connecticut Circle Magazine - 1940). In Connecticut the destruction was equally shocking across the central and eastern half of the state. Much of eastern Connecticut found itself in the dangerous eastern semicircle of the cyclone. Although Long Island offered some modest buffer to the huge ocean surges that hit the south shore of Long Island and Rhode Island - the furious waters of Long Island Sound rose to unimaginable heights. In the beach towns of Clinton and Westbrook, buildings were piled in a mass of wreckage across coastal roads. In the Lymes, many beach cottages were swept away or flattened. Along the shorefront in Stonington, buildings that were swept off their foundations - floated two-miles inland. Many of those killed along the Connecticut coast attempted to stay in flimsy seasonal beach cottages that were only a few feet above sea level. Wind gusts over 120-mph combined with tides up to 12-feet above normal - devastated nearly every coastal community from New Haven to the Rhode Island state line. In the coastal towns to the east of New Haven, the US Postal Service was unable to deliver mail for more than a week. After the 38 hurricane the scene in the City of New London was one of shocking devastation. New London was first swept by the winds and storm surge - then the waterfront business district caught fire - and burned uncontrollably for ten hours. The day after the storm - the Fort Neck section of town was a wasteland of twisted smoldering ruins. The stately beach-front homes along Ocean Beach were leveled by the huge storm surge. The permanently anchored 200-ton lightship at the head of New London Harbor ended up on a sand bar two-miles away. In another unfortunate turn of events - it had been raining for several days before the hurricane hit. The mid - Atlantic States had been in a trough of low pressure for almost a week. The entire week before the 38 hurricane hit - muggy, rainy weather affected the region. The ground quickly became saturated across most of interior Connecticut - and most rivers and streams were nearing bank-full by September 21st. As the 1938 hurricane crossed the Connecticut coast and marched inland - it loosened monsoon-like downpours across Connecticut and Massachusetts. Rainfall of 6 to 8 inches in four hours - sent water cascading down the hilly terrain of interior Connecticut. Several days after the storm hit, the Connecticut River rose to its second highest level ever recorded in Hartford and Middletown. In Hartford, flood waters marooned thousands of people in their homes and business. The East Hartford area had water neck-deep in the street more than a mile from the rivers edge. Thousands were left homeless. A week after the storm, Connecticut reported 97 people killed, over 1000 injured, and several dozen missing. Storm - surge destruction along the eastern Connecticut coast (Stonington) following the 1938 hurricane (2nd Air Base Squadron - Mitchel Field - 1938). Connecticut River at Hartford - 4 times normal width. Arrow at top of photo shows Travelers Insurance Tower. Hundreds of East Hartford homes submerged. Millions in damage. Thousands homeless. (Courtesy of Connecticut National Guard). Although Boston and most of northern Massachusetts escaped any truly severe damage from the 1938 hurricane, the area around New Bedford and Buzzards Bay was heavily damaged. As the storm-surge drove up the narrowing Buzzards Bay, Wareham lay right at the top of the bay. In Onset and Wareham, the wind and waves flattened entire rows of buildings and overturned automobiles. The area around Westport Beach and Horseneck beach was especially hard hit. The day after the storm - Horseneck Beach looked as if had been bombed. Buildings were overturned, the bathhouses and the main road had been swept way, and the coast was littered with debris. The New Bedford Port and docks were in shambles after the storm. In one day - two-thirds of all the boats docked in New Bedford Harbor sunk. Severe inland flooding also occurred in Southbridge and Springfield, with residents stranded for several days after the storm. The true amount of damage from the 38 hurricane will never be known.* Some sections of the Rhode Island coast never recovered from the storm. To this day - several inlets created during the 38 hurricane still persist - along with the slabs and foundations of several buildings. As with any widespread disaster, damage totals and fatalities vary from agency to agency.* The best Red Cross estimates report 600 to 700 killed, 3500 injured, 75,000 buildings damaged, 20,000 automobiles destroyed, and 3,000 boats sunk. The regional power companies collectively estimated that 10,000-miles of electric and telephone wires came down in the storm. The day after the 1938 hurricane slammed into the United States the attention of the world was on major political events unfolding (Hitler invaded Czechoslovakia). It was more than a week before news of the appalling death and destruction along the U.S. Atlantic coast reached the rest of the World. A month after the storm, people were still missing. Although the 1938 hurricane was certainly not the strongest hurricane to hit the United States, the combination of a strong hurricane, moving very rapidly, and striking a densely populated area - created property damage unequaled up to that time. The 1938 hurricane did more damage than the San Francisco earthquake in 1906. According to several publications - the total property damage was the greatest of any natural disaster ever recorded in the Western Hemisphere up to that time. BACK ****© Michael A. Grammatico 1/03************************************************ ************************* * -- This article was auto-posted by the ne.weather.moderated Weatherbot program. The author is solely responsible for its content. ne.weather.moderated FAQ/Charter: http://www.panix.com/~newm/faq.txt ne.weather.moderated moderators e-mail: (Please put "wx" or "weather" in the subject line to avoid the spam block.) |
#2
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The Photos
HURRICANE OF 1938 Address:http://www.geocities.com/hurricanene/hurr1938.htm Changed:9:02 PM on Friday, March 4, 2005 -- This article was auto-posted by the ne.weather.moderated Weatherbot program. The author is solely responsible for its content. ne.weather.moderated FAQ/Charter: http://www.panix.com/~newm/faq.txt ne.weather.moderated moderators e-mail: (Please put "wx" or "weather" in the subject line to avoid the spam block.) |
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