The "Long Island Express": Inside America's Fastest Hurricane

Most hurricanes give people days to prepare. The 1938 New England Hurricane gave them hours, and in some cases, minutes. Nicknamed the "Long Island Express" for its extraordinary forward speed, the storm remains the benchmark against which every hurricane threat to New England is still measured, and understanding why reveals just how dangerous a fast-moving storm can be.

A Hurricane That Outran Its Own Warnings

The storm formed off West Africa in early September 1938 and crossed the Atlantic largely undetected by forecasters, who had no satellites, no radar, and only scattered ship reports to track it with. By the time it was clearly identified as a major hurricane, it was already approaching the Bahamas at near-peak strength.

What made this storm uniquely dangerous wasn't just its intensity, it was its speed. As it approached the East Coast, the hurricane accelerated to roughly 50 mph, one of the fastest forward speeds ever recorded for an Atlantic hurricane. Most storms take days to weaken as they move over cooler northern waters; this one crossed that distance so quickly it barely had time to lose strength, arriving in New England still carrying the power of a major hurricane.

A Forecast That Never Reached the People Who Needed It

Forecasters at the time genuinely believed the storm would curve out to sea, the typical path for hurricanes reaching that latitude. Responsibility for tracking the storm shifted between the Jacksonville and Washington, D.C. weather offices as it moved north, and in the confusion, the New York City office, the one covering the area about to take a direct hit, never received a single detailed update on the storm's location or strength before it arrived.

Early on the morning of landfall, one advisory placed the storm roughly 75 miles southeast of Atlantic City and predicted it would pass over Long Island and Connecticut that afternoon. Later reanalysis showed the storm was actually much closer, stronger, and larger than that advisory described. A 28-year-old junior forecaster named Charles Pierce correctly predicted the hurricane would strike New England directly, based on a trough of low pressure he identified in the data, but he was overruled by senior meteorologists who still expected the storm to turn out to sea. By the time hurricane-force winds arrived, most residents had received no meaningful warning at all.

Landfall at an Extraordinary Speed

The hurricane made its first landfall on Long Island near Bellport at roughly 3 p.m. on September 21, 1938, with sustained winds estimated between 115 and 120 mph, a major Category 3 hurricane. It then crossed Long Island Sound and made a second landfall near New Haven, Connecticut, roughly an hour later, one of only a handful of major hurricanes ever recorded to strike Connecticut directly.

Storm surge proved catastrophic across the region. Narragansett Bay's funnel shape amplified the surge to nearly 16 feet above normal tides, flooding downtown Providence under more than 13 feet of water. Eastern Long Island saw storm tides estimated at 20 feet, essentially turning Montauk into a temporary island and carving entirely new inlets through the barrier islands, several of which, including Shinnecock Inlet, still exist today.

At the Blue Hill Observatory in Massachusetts, sustained winds reached 121 mph with a gust of 186 mph, still recognized as the strongest hurricane-related wind gust ever recorded in the United States.

A Storm That Reshaped the Region

The scale of destruction was staggering. Somewhere between 600 and 800 people died across the Northeast, with additional deaths in Canada as the storm's remnants moved north. Roughly 8,900 homes and buildings were destroyed and another 15,000 damaged. More than 2 billion trees were knocked down across New England and New York, wiping out over a third of the region's forested area and creating a fire hazard so severe that a dedicated federal agency, the Northeastern Timber Salvage Administration, was created specifically to manage the fallen timber.

In New London, Connecticut, downed power lines sparked a fire that burned out of control for ten hours after the storm surge had already devastated the waterfront district. In Westhampton Beach, New York, a wall of water swept across the barrier beach and destroyed 153 of 179 homes, killing 29 people in a single community. A school bus carrying seven children was blown into Mackerel Cove in Jamestown, Rhode Island, killing everyone aboard.

Why the "Long Island Express" Still Matters

Nearly a century later, meteorologists still use this storm as the reference point for worst-case hurricane scenarios in New England, and for good reason. The region's coastline has grown enormously more populated and developed since 1938, and infrastructure that seemed adequate then would face far greater strain from a storm of similar strength today. The Fox Point Hurricane Barrier in Providence, completed decades after the storm, exists directly because of the flooding this hurricane and a later storm caused downtown.

Modern forecasting technology means a storm like this would never again arrive as a near-total surprise. But the storm's core lesson, that a hurricane's forward speed can matter just as much as its wind speed in determining how much warning people actually get, remains directly relevant to how forecasters communicate hurricane threats along the East Coast today.

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