The Great Lakes Storm of 1913, historically referred to as the Big Blow, the Freshwater Fury and the White Hurricane, was a blizzard with hurricane-force winds that devastated the Great Lakes region in the Midwestern United States and Southwestern Ontario, Canada, between November 7 and 10, 1913. The storm was at its most powerful on November 9, battering and overturning ships on four of the five Great Lakes, particularly Lake Huron.
With more than 250 people killed, the storm was the deadliest and most destructive natural disaster to hit the Great Lakes in recorded history. Shipping was hard hit; 19 ships were destroyed, and 19 others were stranded. About 68,300 tons of cargo—including coal, iron ore, and grain—were lost. Damages were estimated at nearly $4.8 million ($162 million in 2026). The storm impacted many cities, including Duluth, Minnesota; Chicago, Illinois; and Cleveland, Ohio. Cleveland received 22 in (56 cm) of snow combined with winds up to 79 mph (127 km/h) and was paralyzed for days.
The extratropical cyclone originated when two major storm fronts fueled by the Great Lakes' relatively warm waters—a seasonal process called a "November gale"—converged. It produced wind gusts of 90 mph (140 km/h), waves estimated at over 35 feet (11 m) high, and whiteout snowsqualls. Winds exceeding hurricane-force occurred over four of the lakes for extended periods, creating very large waves. The large size of the lakes provides wind fetches (the length of water over which a given wind has blown without obstruction) of hundreds of miles, allowing huge waves to form. Rogue waves are known to occur on the Great Lakes, including waves reinforced by reflections from the vertical shores of some of the lakes.
The United States Weather Bureau, precursor to the National Weather Service, failed to predict the intensity of the storm, and the process of preparing and communicating predictions was slow. These factors contributed to the storm's destructiveness. The contemporaneous weather forecasters did not have enough data, communications, analysis capability and understanding of atmospheric dynamics to predict the storm. They could not predict wind directions, which is key to the ability of ships to avoid or cope with the effects of storms.
Background
The water in the five Great Lakes holds heat that allows them to remain relatively warm late into the year and postpones the cooling and first frosts in the region. During the autumn, two major weather tracks converge over the area. Cold, dry air moves south and southeast from northern Canada as an Alberta clipper, while warm, moist air moves north and northeast from the Gulf of Mexico along the lee of the central Rocky Mountains as a Colorado low. The collision of these air masses forms large storm systems in the middle of the North American continent, including the Great Lakes. When the cold air from these storms moves over the lakes, it is warmed by the waters below and picks up a spin. As the cyclonic system continues over the lakes, its power is intensified by the jet stream above and the warm waters below.
The resulting storm, which is commonly called a "November gale" or "November witch", can maintain hurricane-force winds, produce waves over 50 feet (15 m) high and dump significant falls of rain or snow. Fueled by the warm waters, these powerful storms may remain over the Great Lakes for days. November gales have caused several large storms over the Great Lakes, with at least 25 killer storms affecting the region since 1847. During the Mataafa Storm in 1905, 27 wooden vessels were lost. During a November gale in 1975, the giant bulk carrier SS Edmund Fitzgerald sank suddenly without sending a distress signal and with all crew still on board. The large size of the lakes provides fetches of hundreds of miles allowing huge waves to be developed. Their large unobstructed spaces result in wind speeds higher than nearby inland areas. Rogue waves (including a phenomenon named the "Three Sisters") are known to occur on the Great Lakes, including waves reinforced by reflections from the vertical shores of some of the lakes. Waves on the lakes (especially the shallower ones) can be steeper and closer together than on the ocean, allowing less recovery time between waves. Compared to the ocean, the Great Lakes also have less maneuvering "sea room" and closer proximity to shores, making it more difficult for ships to weather storms.
Weather forecasting
At the time of the storm, the United States Weather Bureau did not have enough data, communications, analysis capability and understanding of atmospheric dynamics to predict or understand the storm. They also were unable to predict wind directions to allow ships to avoid or cope with the storm's conditions. More modern studies of the available information and data from the storm provide better descriptions of its weather mechanisms and treat it as two storms.
Weather forecasters of the time did not have enough data or understanding of atmospheric dynamics to predict or comprehend the events of Sunday November 9. Frontal mechanisms, which were then referred to as "squall lines", were not yet understood. Surface observations were only collected twice daily at stations around the country; by the time these data were collected and maps were hand-drawn, the information was no longer representative of the actual weather conditions.
Prelude
The Great Lakes Storm of 1913 was first noticed on Thursday, November 6 on the western side of Lake Superior, moving rapidly toward northern Lake Michigan. The weather forecast in The Detroit News predicted "moderate to brisk" winds at the Great Lakes with occasional rain on Thursday night or Friday for the upper lakes (except southern Lake Huron) and fair-to-unsettled conditions for the lower lakes. Around midnight on November 6–7, the steamer Cornell, which was 50 miles (80 km) west of Whitefish Point in Lake Superior, ran into a sudden northerly gale and was severely damaged. This gale lasted until late November 10 and almost forced Cornell ashore.
Storm
By November 7, a string of low-pressure centers in Canada had consolidated into a low-pressure center southwest of Lake Superior which became "Storm #1". At the same time, warm air pushed into the central Great Lakes from the south. By November 8, this storm was moving east through northern Lake Huron while strong northerly winds developed behind it over Lake Superior. By November 9, "Storm #2" had formed over the Carolinas and Virginia. The northern portion of this storm began sweeping warm moist Atlantic air over colder air in the Ohio area producing heavy snows. The northwest portion of this extremely powerful storm began creating strong winds from the north along the long axis of Lake Huron, building large waves. By November 10, 24 hours of such building had created immense waves which ships were subjected to along with the high winds as the center of the storm crossed north/northwest over Lake Erie toward Toronto. Surface pressures went as low as 968.5 hectopascals (millibars), the lowest of the storm.
Winds exceeding hurricane-force occurred over four of the Great Lakes for extended periods. Wave heights observed during the storm were estimated by observation rather than measurement; observations of regular waves exceeding 35 ft (11 m) were corroborated by modern-day simulations which estimate these at 38 ft (12 m). Interaction between waves (such as those reflected from vertical shorelines) can nearly double wave heights; observations of such waves during the storm estimated some as high as 50 ft (15 m).
November 7
On Friday, the weather forecast in the Port Huron, Michigan, Times-Herald described the storm as "moderately severe". The forecast predicted increased winds and falling temperatures over the next 24 hours. At 10:00 a.m., United States Coast Guard stations and all 112 Weather Bureau signal stations on the Great Lakes received a directive to hoist a square, red signal flag with a black center and a red, triangular maritime pennant below it, indicating a storm with winds of 55 mph (89 km/h) that would blow from the southwest. After dark, a red lantern over a white one was displayed to warn of storm winds from the west. The winds on Lake Superior had already reached 60 mph (97 km/h), with gusts to 80 mph (130 km/h), and an accompanying blizzard was moving toward Lake Huron. Sustained wind speeds reached 62 mph (100 km/h) and gusts to 68 mph (109 km/h) at Duluth.
November 8
By Saturday, the storm's status had been upgraded to "severe". At 10:00 a.m., Coast Guard stations and Weather Bureau offices at Lake Superior ports raised white pennants above red and black storm warning flags, indicating a storm warning with northwesterly winds. The storm was centered over eastern Lake Superior, covering the entire lake basin. The weather forecast of the Times-Herald stated southerly winds had remained "moderate to brisk". Northwesterly winds had reached gale strength on northern Lake Michigan and western Lake Superior. Gale wind flags were raised at more than 100 ports, but many captains continued their journeys. Long ships traveled through the St. Marys River all that day, through the Straits of Mackinac all night, and up the Detroit and St. Clair rivers early the following morning.
The 472 feet (144 m) steel bulk freighter L. C. Waldo, 18 hours out of Two Harbors, Minnesota, was overrun by monster waves out of the northwest on Lake Superior. Approximately 45 miles northeast of Keweenaw Peninsula, an estimated 50 ft (15 m) rogue wave smashed the wheelhouse; bent the steel floor of the compass room; swept the wheelsman out of the wheelhouse; and tore three of the walls from the Texas (the level of the deck house below the wheelhouse). The captain ordered that the ship be turned around to try to reach shelter behind the Keweenaw Peninsula. As recounted by second mate Feeger: "The wind sent one gigantic wave after another over parts of the ship...The snow was so blinding that none of us could see 50 feet ahead". Waldo's rudder then failed; helpless without it, 70 mph (110 km/h) winds drove the ship aground on Gull Rock near Manitou Island. With the bow wedged in the rocks, the hull shredded, and a crack forming in the deck, the captain ordered everyone to the bow and to flooded ship to prevent her from being washed back into the depths of the lake. The steward's wife and her mother were reluctant to leave the stern, and the crew struggled to carry them over hundreds of feet of open deck in the storm, including traversing a widening crack. During the process the chief engineer and two stokers ran the ship at full power to try to wedge the bow further onto the shore. They then abandoned the stern and took shelter with the others in the unheated windlass room.
November 9
By noon on Sunday, barometric pressures in some areas began to rise, bringing hopes of an end to the storm. The low pressure area that had moved across Lake Superior was moving northeast, away from the lakes. The Weather Bureau issued the first of its twice-daily reports at approximately 8:00 a.m.; it did not send another report to Washington, D.C., until 8:00 p.m. This proved to be a serious problem; the storm would have most of the day to build up hurricane-force winds before the Bureau headquarters in Washington would have detailed information.
Along southeastern Lake Erie near Erie, Pennsylvania, a southern low-pressure area was moving toward the lake. This low had formed overnight so was absent from Friday's weather map. It had been moving northward but turned northwestward after passing over Washington. The low's intense, counterclockwise rotation was made apparent by the changing wind directions around its center. In Buffalo, New York, morning northwest winds had shifted to the northeast by noon and to the southeast by 5:00 p.m., with gusts of up to 80 mph (130 km/h) occurring between 1:00 p.m. and 2:00 p.m. In Cleveland, Ohio, 180 miles (290 km) to the southwest, winds remained northwest during the day, shifting to the west by 5:00 p.m., and maintaining speeds of more than 50 mph (80 km/h). The fastest gust in Cleveland, 79 mph (127 km/h), occurred at 4:40 p.m. At Buffalo, barometric pressure dropped from 29.52 inHg (999.7 hPa) at 8:00 a.m. to 28.77 inHg (974.3 hPa) at 8:00 p.m.
The rotating low continued northward into the evening, bringing its counterclockwise winds in phase with the northwesterly winds already hitting Lakes Superior and Huron. This resulted in a dramatic increase in northerly wind speeds and swirling snow. Ships on Lake Huron that were south of Alpena, Michigan—especially around Harbor Beach and Port Huron—experienced massive waves moving southward toward St. Clair River. Some ships sought shelter along the Michigan shore or between Goderich and Point Edward, Ontario. Three of the larger ships were found capsized, indicating extremely high winds and tall waves. From 8:00 p.m. to midnight, the storm became a "weather bomb" with sustained hurricane-force winds of more than 70 mph (110 km/h) on the four western lakes. The worst damage was done on Lake Huron as ships sought shelter along its southern end. Gusts of 90 mph (140 km/h) were reported off Harbor Beach. The lake's shape allowed northerly winds to increase unimpeded.
November 10 and 11
The storm had moved northeast of London, Ontario, by Monday morning, with lake effect blizzards behind it. An additional 17 inches (43 cm) of snow fell on Cleveland that day, filling the streets with snowdrifts 6 feet (180 cm) high. Streetcar operators stayed with their stranded, powerless vehicles for two nights, eating food provided by local residents. Travelers were forced to take shelter and wait for the storm to pass.
By Tuesday, the storm was rapidly moving across eastern Canada. Without the warm lake waters, it quickly lost strength. The system carried less snowfall because of its speed and the lack of lake effect snow. All shipping along the St. Lawrence River around Montreal was halted on Monday and part of Tuesday.