1938 New England hurricane in the context of Great Colonial Hurricane of 1635


1938 New England hurricane in the context of Great Colonial Hurricane of 1635

⭐ Core Definition: 1938 New England hurricane

The 1938 New England Hurricane (also referred to as the Great Long Island - New England Hurricane and the Long Island Express) was one of the deadliest and most destructive tropical cyclones to strike the United States. 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 Wednesday, 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 2024). Also, numerous others estimate the real damage between $347 million and almost $410 million. Damaged trees and buildings were still seen in the affected areas as late as 1951. It remains the most powerful and deadliest hurricane to ever strike New York State and New England in history, perhaps eclipsed in landfall intensity only by the Great Colonial Hurricane of 1635.

The storm developed into a tropical depression on September 9 off the coast of West Africa, but the United States Weather Bureau was unaware that a tropical cyclone existed until September 16 when ships reported strong winds and rough seas 350 miles northeast of San Juan; by then, it was already a well-developed hurricane and had tracked westward toward the southeastern Bahamas. It reached hurricane strength on September 15 and continued to strengthen to a peak intensity of 160 mph (260 km/h) near the southeastern Bahamas four days later, making it a Category 5-equivalent hurricane. The storm was propelled northward, rapidly paralleling the East Coast before making landfalls on Long Island and Connecticut as a Category 3 hurricane on September 21, with estimated sustained winds of 115–120 mph. After moving inland, it transitioned into an extratropical cyclone and dissipated over Ontario on September 23.

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1938 New England hurricane in the context of Shinnecock Bay

Shinnecock Inlet is the easternmost of five major inlets connecting bays to the Atlantic Ocean through the narrow 100-mile-long (160 km) Outer Barrier that stretches from New York City to Southampton, New York on the south shore of Long Island. It splits Westhampton Island from the peninsula extending from Southampton Village. The inlet was formed by the 1938 New England hurricane, which killed several people when it permanently broke through the island in Hampton Bays, New York. The name comes from the Shinnecock Indian Nation.

Maintenance of the inlet has been controversial. It saves boaters in the Hamptons several miles in access to the Atlantic Ocean. The inlet is almost directly lined up with the Shinnecock Canal between Shinnecock Bay and the Peconic Bay, which allows a shortcut to the ocean for boaters on the North Fork of Long Island.

View the full Wikipedia page for Shinnecock Bay
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