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Ecology · Climate history

Weather, Severe Events

A chronicle of notable blizzards, floods, and hurricanes whose winds, snow, rain, ice, and coastal effects have shaped Maine.

Blizzards, floods, and hurricanes are occasional weather events in Maine, but their arrival can be sudden and severe. The historical record shows how geography, season, snowpack, wind, and water combine to create damaging conditions.

Snow and wind

Blizzards

November 26, 1898, was the first day of the two-day Portland Gale, a hurricane and blizzard that raged for more than thirty-six hours. It sank about one hundred vessels, including the steamer Portland, which was lost off Massachusetts. The wreck took 192 lives.

Maine experienced many substantial blizzards during the twentieth century. Two closely timed storms were described in a historical account from the Brunswick Times Record:

December 28–29, 1922: Snow buried broad areas beneath drifts eight feet high or more. On exposed roads without snow fences, trees, or shrubs, some drifts reportedly reached 20 feet.

January 12, 1923: Another severe storm brought gale-force winds of 25 to 35 mph. By the middle of January, seasonal snowfall in the area had reached 70 inches.

The following table summarizes several major twentieth-century snowstorms reported in the historical record.

DateRecorded impact
February 25–27, 1934A 68-hour storm left 22.7 inches of snow in Portland. Temperatures remained between 7 and 16 degrees, and much of Portland Harbor froze.
January 23–24, 1935Portland received 23.3 inches of new snow, with temperatures of 8 to 12 degrees and wind gusts reaching 35 mph.
December 27–28, 1946Twenty-one inches fell in Portland amid temperatures from 0 to 12 degrees and gusts of 35 mph.
February 17–18, 1952Known as “The Great Blizzard,” the storm brought 25.3 inches to Portland and about three feet to northern Maine. Winds gusted to 65 mph.
February 9–10, 1969A two-day storm added 21.5 inches in Portland while winds gusted to 54 mph.
December 17–18, 1970Nearly 23 inches of snow fell in Portland over two days.
February 6–7, 1978Southern Maine received roughly 8 to more than 12 inches. Gusts exceeding 100 mph created severe blowing and drifting snow.
January 17–18, 1979A record 27.1 inches fell in Portland with gusts of 46 mph; 24.1 inches accumulated within 24 hours.
Rivers and runoff

Floods

Rainfall in Maine is generally distributed across the year, but many historically damaging floods have occurred from late winter through spring. During that period, rainfall can combine with frozen ground, melting snow, full rivers, and ice jams.

After several days of intense rain, floods on June 19, 1814, swept away bridges and other structures in Kennebunk, Fryeburg, and Brownfield, as well as along the Androscoggin River in Brunswick and Topsham.

A notable autumn exception was the “Great Freshet of October 1785,” which swept away nearly all mills and bridges in Berwick and Kennebunk.

DateArea affectedContemporary damage estimate
March 19, 1936South-central Maine$25,000,000
March 27–30, 1953Southwestern MaineNo figure listed
May 28, 1961Eastern Maine$1,000,000
April 30, 1979Northern Maine, St. John River basin$650,000
April 1, 1987Central and south-central Maine$100,000,000
April 10–12, 1991Northern Maine, St. John River basin$14,400,000
October 20–22, 1996Southwestern Maine$6,450,000 estimate
Reading historical figures: These are estimates recorded in period sources and are presented in the dollar values reported at the time, without adjustment for inflation.

Warm frontal systems can bring abundant rainfall northward while frozen ground absorbs little water. Rivers may already be near their banks because of snowmelt, and remaining snowpack can add substantially to runoff. These floods often develop more slowly than summer flash floods, yet last longer and cover larger areas.

Ice jams can make the effects more destructive. Jams on the Kennebec River contributed to severe damage during the 1936 flood. In 1991, an ice jam on the St. John River near Allagash destroyed two bridges.

Tropical systems

Hurricanes

Maine lies far north of the regions most frequently struck by tropical cyclones, but hurricanes and their remnants have repeatedly brought destructive rain, wind, coastal water, and power loss to the state.

DateEvent and recorded effects
August 1635A probable major hurricane affected early English settlements in New England.
October 19, 1775A hurricane brought three days of rain and flooding to the expedition marching toward Quebec.
March 12, 1888The Blizzard of 1888, called the “Great White Hurricane,” paralyzed much of the East Coast from Chesapeake Bay to Maine.
November 26, 1898The first day of the two-day Portland Gale, both a hurricane and a blizzard.
September 21, 1938The New England Hurricane caused reported damage in Maine.
September 15, 1944The Great Atlantic Hurricane reached Maine with hurricane-force impacts.
September 7, 1953Hurricane Carol caused minor wind damage around Eastport.
August 31, 1954A later storm also named Carol brought flooding rain and winds measured at 69 mph in Portland.
September 11, 1954Hurricane Edna arrived eleven days later, damaging Maine’s apple crop and other property.
September 12, 1960Hurricane Donna uprooted trees and sank pleasure craft along the coast.
October 29, 1963Hurricane Ginny brought gusts reported near 100 mph in Rockland and 6 to 18 inches of snow in western mountain areas.
August 19, 1991Hurricane Bob produced gusts of 61 mph in Portland, prolonged power outages, and three deaths in Maine.

Sources and editorial notes

  • Historical storm summaries reported by the Maine Sunday Telegram, November 6, 2006.
  • Flood information compiled from USGS Water Supply Paper 2375 and the Maine Emergency Management Agency.
  • Flood-process context attributed in the source record to the Maine Geological Survey.
  • “A Century of Photos,” Supplement to the Times Record, January 31, 2014.
  • Historical cyclone chronology based on a New England tropical cyclone climatology covering 1938–2004.
Understanding the pattern

Why spring flooding can become severe

No single factor explains every flood. The largest events often develop when several seasonal conditions overlap across a river basin.

Fast-moving river swollen by rain and seasonal runoff
Heavy rainfall

Warm weather systems can carry sustained rain into the state.

Frozen ground

Water runs over soil that cannot readily absorb it.

Snowmelt

Warming temperatures release stored water across a watershed.

Ice jams

Moving river ice can obstruct flow and rapidly raise water levels.

FAQ

Reading the severe-weather record

Answers to common questions about the dates, measurements, and organization of this historical entry.

What kinds of events are included here?

The entry focuses on historically significant blizzards, river floods, hurricanes, and tropical systems that affected Maine.

Are the historical damage estimates adjusted for inflation?

No. Dollar figures are reproduced as contemporary estimates from the cited historical record and should not be compared directly without further economic analysis.

Why do many major floods occur in spring?

Spring rain may coincide with frozen soil, melting snow, high river levels, and mobile river ice. Several of these conditions can affect a large watershed at once.

Can hurricanes affect Maine after weakening?

Yes. A tropical cyclone or its remnants can still carry heavy rain, strong winds, large waves, and coastal water into Maine even after losing peak tropical intensity.

Why do some measurements focus on Portland?

Long-running observations and newspaper accounts make Portland a frequent reference point. Conditions elsewhere in Maine may have differed substantially during the same storm.

Where can I explore related climate topics?

Use the linked weather overview, climate category, river category, historical dates, and map browser to continue through related entries.

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