Type | Blizzard Winter storm |
---|---|
Formed | December 10, 1944 |
Dissipated | December 13, 1944 |
Maximum snowfall or ice accretion | 36.0 inches (91 cm) - recorded at Elkins, Randolph County, in West Virginia |
Fatalities | 87-100 fatalities in United States and 21-24 in Canada |
Areas affected | Eastern Great Lake States and Provinces of North America |
The Great Snowstorm of 1944 [lower-alpha 1] was a disruptive winter storm that brought high winds and between 12 and 30 inches (30 and 76 centimetres) of snow to the eastern Great Lakes region of North America between Sunday, December 10, and Wednesday, December 13, 1944. The areas most affected included northeastern Ohio, western Pennsylvania, West Virginia, upstate New York, southern Ontario and southern Quebec.
The snowstorm was caused when two separate storms, one from the west, which had dropped moderate amounts of snow through the Central Great Plains and Midwest of the United States, and another from the southern Atlantic Coast, both moved towards Pennsylvania, causing high snowfall amounts and high winds in the adjacent states and provinces, before both moved easterly through New England and then into the Atlantic Ocean. [1] [9] [10] Other effects of the twin-pronged storm, such as cold temperatures, high winds, light snow, sleet, freezing rain and rain, covered the remainder of the eastern United States and southern central Canada. [11] [12]
Including the toll from the western storm, the death toll was between 87 and 100 people in the US and between 21 and 24 people in Canada, with an unknown total of serious injuries. The most heavily impacted major cities included: Toronto with 57.2 cm (22.5 in) of snow; Hamilton, Ontario, with 62.5 cm (24.6 in); Pittsburgh with 15.5 inches (39 cm); and Rochester with 22.3 inches (57 cm); while smaller cities with the greatest snowfalls included St. Catharines, Ontario, with 66 cm (26 in) and Erie, Pennsylvania, with 26.5 inches (67 cm).
The storm was crippling to these urban areas such that most car, truck, streetcar and bus transport was blocked for a full day and hindered for three to five days, while stores, government offices and factories were closed for one to two days, and schools were closed for two to three days or longer. In some rural areas nearby these cities, people were snowbound to varying degrees for up to five or six days. Intercity travel by road, bus or air was blocked for two to three days and train travel was blocked or subject to long delays for one to two days. The single highest snowfall was recorded in Elkins in Randolf County, West Virginia, which received 36 inches (91 cm), with other mountainous areas of that state receiving about 30 inches (76 cm).
One low pressure system/storm had formed late on December 8 in the southern High Plains and, drawing in cold air from the north, slowly moved northeastward producing snowfall over a large area, including as far south as the northern portions of some Gulf States. [9] [11] States receiving substantial snowfalls included Colorado, Kansas, Nebraska, Missouri, Iowa, Illinois, southern Wisconsin, Kentucky, Indiana and southern Michigan. [9] [11] A smaller low pressure system/storm, containing warm moist air, formed along the southern Atlantic Coast late on December 10 and unexpectedly moved northward towards Pennsylvania on December 11, slowing down the storm from the west and bringing additional moisture, thereby increasing snowfall amounts in the adjacent states and provinces in the eastern Great Lakes Region plus southward along the spine of the Appalachian Mountains. [1] [9] [10]
Cities such as Pittsburgh and Toronto were expecting four or five inches of snow but instead received four to five times that amount, leading Pittsburghers to call it the "sneak" snowtorm. [10] [13] Winds whipped snow into drifts and impeded traffic considerably over much of the affected areas. [9] On December 12, the storms moved northeasterly to northern Maine leaving snow across much of their wake with the highest amounts being in northeastern Ohio, western Pennsylvania, West Virginia, western, central and northern New York, southern Ontario and southern Quebec. [14] The East Coast received winds gusting to 73 miles per hour (118 kilometres per hour) along with precipitation ranging from a light slush in Washington to freezing rain in parts of New England. [15] The temperatures in the area of greatest snowfall were about normal, but substantially colder than normal temperatures were experienced throughout the southeastern United States, such that 5 inches (13 cm) of snowfall fell in North Carolina, light snowfall occurred in Mississippi, Alabama and Georgia, and citrus crops were threatened in central Florida. [12] [14] [16]
The societal impact of the Great Snowstorm was assessed by the National Weather Service of the US as having Regional Snowfall Index (RSI) value of 9.504 in the Ohio Valley Region [17] and 2.155 on the Northeast Region, [18] while its two initiating storm systems had an RSI of 1.784 on the Upper Midwest [19] and 1.989 on the Southeast. [20] The ranking in the Ohio Valley Region labels it as a Category 3 ("Major") snowstorm while the rankings in the other three regions were as a Category 1 ("Notable") snowstorm. The total RSI of the storm is 15.3 which would rank it as a Category 4 ("Crippling") Snowstorm, the second highest category after Category 5 ("Extreme"), and place it seventh all-time in the RSIs for snowstorms in the Northeast. [18] As well, the area of snowfall of 12 inches (30 cm) or greater affected more people than all snowstorms in the Ohio Valley Region between 1932 and 1967 aside from the Great Appalachian Storm of November 1950. [21]
The impacts of the snowstorm on southern Ontario and southern Quebec in Canada are not accounted for in the U.S. National Weather Service's RSI. [18] The snowfall received by downtown Toronto and surrounding areas is the highest from any storm since 1872 and among the highest in history for most other cities in the Golden Horseshoe at the western end of Lake Ontario, although other winter storms are considered to have had a greater impact on southwestern Ontario (see Great Blizzard of 1978), eastern Ontario [22] and the southern portions of the Niagara Peninsula (see Blizzard of 1977), and the Blizzard of 1999, together with snowstorms which affected Toronto over the following 14 days, may have had a greater accumulative impact on Toronto.
Final tallies of fatalities from the combined storm system ranged from 87 to 100 for the US [1] [23] [24] and 21 to 24 for Canada, all of Canada's being in southern Ontario. [5] [25] [26] [27] The deaths in the US occurred in at least 16 states from Colorado in the west and Arkansas in the south, to Maine in the northeast, with Pennsylvania, Ohio, New York and Michigan having the greatest number. [28] [29] [30] [31] [32] [33]
The exact causes of death in the Midwest and Great Plains states (Indiana and westward) were predominantly vehicular accidents, whereas for Michigan about half of the fatalities were on account of vehicular accidents. [11] [34] [33] For Ohio, southern Ontario, western Pennsylvania and western New York, the areas which had the quickest snowfall and, generally, the highest snowfall—which resulted in roads that were largely physically undriveable until they were properly plowed—causes aside from vehicular accidents were prevalent, these including: heart attacks from exhaustion from struggling to walk through snow drifts in blizzard conditions, or from shovelling or pushing cars out of snow drifts or from the stress of a car being stuck in the snow, or from shovelling in general; sledding ("coasting") accidents, including colliding with moving vehicles; vehicles hitting pedestrians, who in some cases were walking on roads as sidewalks were unwalkable; a streetcar overturning; exposure to the cold; electrocution by wires that fell due to high winds; and, death from traumatic, delayed child birth (see the below sections for these four jurisdictions for details on fatalities and references). In the 21st century, some of these, such as shovelling not involving a trapped car or sledding, are classified by some sources as "indirect" rather than "direct" deaths from a snowstorm.
Numerous injuries from causes similar to the fatalities, plus from falls, were reported in various newspapers, but only for Toronto was a tablulation reported, which was of about 100 serious injuries, including 54 fracture cases, for the 30 hours of the storm. [25] [27] [35] In Pittsburgh, in the 24 hours at the height of the snowstorm, severe injuries reported (i.e. fractures and internal injuries) included six people when a trolley hit a transport truck, a bus driver in a collision, four workers or pedestrians hit by vehicles, one person from a fall, and three youngsters from sledding accidents. [36] [37] [38] Amongst cities impacted by the western storm, Chicago reported "scores of injuries from falls", including one cracked skull, and two severe injuries from a car-subway train collision, in one 24-hour period from December 10 to 11, during which time four deaths also occurred. [39] In St. Louis, a major hospital reported 30 people had required treatment for injuries suffered from falls on icy sidewalks or roads in one 24-hour period, and in a second 24-hour period, six severe fracture cases from falls, including a skull fracture (which resulted in death), were reported. [40] [41] [32]
While Cincinnati and Toledo received 4.5 and 4 inches (11 and 10 centimetres) of snow, respectively, from the storm on December 11, snowfalls rose to 9.7 inches (25 cm) in Cleveland, 11.5 inches (29 cm) in Akron and 14.8 inches (38 cm) in Youngstown in the northeast of the state where the snow carried over into December 12. [42] [43] [44] Forty mph (64 km/h) winds created blizzard conditions in some areas and blew the snow into high drifts which completely blocked many major highways for one to two days and secondary highways for two or three days. [45] [46] [47] Near the northwest town of Waterville, 50 vehicles, including trucks, buses and private automobiles, were stranded in one section of highway. [46] Intercity bus transportation was halted for two days, with reported 15-foot (4.6-metre) banks blocking buses from Cincinnati from reaching Columbus and a State Highway Official stating much of their road-clearing equipment had been damaged by futile attempts to remove such high drifts. [48] [49]
Most trucking lines were brought to a standstill, with one company indicating 180 of their trucks were either stuck in snow near or waiting in Akron until they could proceed. [48] In Akron, 110 of the city's 131 buses were mired in snow drifts at one point on December 12 and taxi companies pulled their cars from the road at 1 p.m. that day; bus service did return to 90% until late December 13. [44] [46] Towing companies estimated to callers that there was a seven-hour wait to tow cars, chiefly because many of their tow tucks had themselves gotten stuck in the snow; with so many people stranded downtown, people stormed hotel desks to get rooms for the night. [44]
Trains arriving in Ohio cities were between two and twelve hours late on December 12 and many were late on December 13 as well. [48] [50] [51] Air travel from northeastern Ohio airports, such as Cleveland, Akron and Youngstown, was halted for December 12 and part of December 13, and the Cleveland evening newspapers did not publish their late editions for December 12. [45] [51] Several major war plants were shut down for December 12, including those in Youngstown, Sandusky and Chillicothe, and electricity and telephone communication were out in numerous counties. [44] [46] Twelve people were killed in Ohio on account of the storm, specific causes including heart attacks from pushing vehicles out of snow drifts or the stress of being mired in snow drifts, pedestrians being hit by skidding motor vehicles, being an occupant of crashing vehicles, and electrocution (one person). [51] [52] [53]
Large areas of western Pennsylvania received a foot of snow or more from the Great Snowstorm, with Titusville and Warren in the inland northwest, receiving 26 and 18 inches (66 and 46 centimetres) of snow, respectively. [1] [54] Coupled with high winds, keeping the area's highways clear became very difficult, prompting the State Highway Superintendent to state "we're getting nowhere," adding that as fast as they plowed the roads the snow drifted back over them. [54] [55] Thousands of vehicles were stranded along highways and country roads, including hundreds of transport trucks and many cars on the Pennsylvania Turnpike—many of the occupants of these vehicles which needed to get shelter at nearby farm houses or service centres until the Turnpike was cleared almost a day later. [55] [56] [57] Hundreds of deer hunters were trapped in the forest belts northeast of Pittsburgh and had to spend four to five days sheltering in hunting cabins or in trailers, trucks or automobiles, with one being found unconscious in a snow drift with their legs badly frozen. [58]
Once the snow stopped on December 13, the winds increased, gusting to 73 mph (117 km/h), which turned the streets that had been a least partly cleared and had turned slushy, into hard bumpy, ridges of ice, further crippling transportation. [1] The storm's death toll in western Pennsylvania was 16, including 15 in the Pittsburgh District and one in the City of Erie, the latter being a person found dead in his marooned car. [1] [54] [59] When the storm moved easterly, the precipitation changed to rain or freezing rain in most of central and eastern Pennsylvania, with one death and one severe injury occurring in Philadelphia when two workers spreading sand at an ice-covered intersection were hit by a car. [56] [60]
The storm unexpectedly deposited 10.3 inches (26 cm) of snow on Erie the afternoon and evening of Monday, December 11, followed by a further 16.2 inches (41 cm) on Tuesday, December 12—a total of 26.5 inches (67 cm)—leaving the City completely isolated, industry crippled and commerce at a standstill. [43] [54] Described as the "most paralyzing storm in Erie's history", 50 m/hr winds whipped the snow into 5- and 6-foot (1.5-1.8 metre) drifts. [54] Local bus service was halted the night of December 11; many buses never made it back to the garage and plows sent out to rescue them got stalled in snow drifts as well. [54] [61]
By late December 12, some buses began running again and by the morning of December 13, half of the fleet was operating, although some were still getting stuck, requiring their riders to get out to push them out of snow drifts. [62] On December 14, while intercity buses began running again, most of the city's streets, as well as nearby suburban highways and country roads, remained clogged—bulldozers were needed to tackle many of them as snow plows alone could not do it. [63] Later on December 14, after another 3.4 inches (8.6 cm) of snow fell on Erie, the Mayor declared a State of Emergency and requested additional snow-clearing equipment from the state as, although city buses were able to run, most private transportation was still inoperable. [1] [43] [55] [64] Schools in Erie only reopened on Monday, December 18, after being closed for four school days. [63]
Heavy snow hit Pittsburgh in the early afternoon of December 11 and by dinner-time transportation in the city was crippled; streetcars, trolleys and buses were immobile and auto traffic on roads leaving the downtown was at a standstill due to accidents and deep snow. [10] [36] [65] Thousands of office workers and Christmas shoppers were trapped downtown for the night—as all hotels filled up rapidly, the stranded people ended up spending the night sleeping in hotel lobbies and ballrooms, railroad stations, bus stations and the County Courthouse. [36] [65] [66] Some people spent 4 to 5 hours walking home, many using the automobile and streetcar tunnels through Mount Washington on the west side of the Monongahela River, which were otherwise unused since cars and streetcars could not get to them. [36] War plant workers could not get home so they stayed overnight and the next shifts could not get in, so production slumped significantly, and 24 mines in the District were closed on December 12. [10] [12]
The 10.7 inches (27 cm) of snow Pittsburgh received on December 11 remains the second highest single-day snowfall in the city's history; including December 12, the storm deposited 15.0 inches (38 cm). [67] Removing the snow was a major problem for Pittsburgh—the City dumped thousands of truckloads of snow from the city's downtown into the Allegheny and Monongahela Rivers but it still took four days until most downtown streets were clear. [68] [69] [70] Clearing the streets was impeded by thousands of vehicles marooned along downtown and suburban streets and on country roads and highways even two days after the storm. [71] On December 12, streetcars were running, although behind schedule, but it wasn't until December 14, the same day schools and Universities reopened after being closed two days, that trolley and buses were able to provide somewhat regular service. [36] [72] [73] [74] Air travel in and out of Pittsburgh was suspended from December 11 until December 14 and intercity bus, car or truck travel was minimal for two days until highways could be properly plowed. [10] [70]
Residential streets were not cleared for several days during which time regular deliveries of coal to homes were impossible. [72] In the cases of sick or disabled persons or other emergency need for coal, the coal companies were undertaking emergency coal deliveries, but were sometimes thwarted due to snow banks blocking residential streets and driveways. [75] Some rural townships just outside the City of had a very difficult time plowing all the local country roads; scores of families in one Township, some needing medical attention and others faced with only minimal food, remained snowbound three to four days after the storm due to snow too deep for the Township's plows. [59] Fifteen people died in the Pittsburgh District, most from heart attacks from shovelling or pushing or digging cars out of snow, but some were pedestrians being hit by vehicles and a few were found dead in marooned cars. [57] [59] [72] [76] Two houseboats in Pittsburgh sank due to heavy snow but no injuries were inflicted. [52]
Clarksburg, received 19 inches (48 cm) of snow but other areas of West Virginia received 30 inches (76 cm) of snow on December 12, with the peak snowfall in North America (36 inches/91.4 cm) occurring in Ekins in Randolf County, that area's highest snowfall in half a century. [52] [14] [77] As roads and highways were generally impassible, particularly through the Appalachian Mountains, all buses throughout the state were cancelled, most schools were closed, mines shutdown, and in parts of the state, the storm snapped telephone and electricity lines. [28] [65] A two-coach passenger train was missing for over a day in snow banks about 45 miles (72 km) west of Charleston and a rescue train itself got marooned in deep drifts and broken tree branches 10 miles (16 km) short of the first train. [78] [52] The adjacent parts of northwestern Maryland were similarly affected, with as much as 15 to 20 inches (38 to 51 centimetres) of snow and drifts of 10 feet (3.0 metres), caused by 40 m/ph (65 km/h) winds, blocking several highways. [29] [79] One person died from exposure in the western part of the Maryland and two people died and several others were seriously injured in vehicle crashes, one involving a bus, caused by icy roads elsewhere in the state. [29] Parts of Virginia's northern and western sections also received substantial amounts of snow and primary highways were not able to be cleared until December 14 at which time secondary highways were still blocked. [80]
Beginning with 4 to 5 inches (10 to 13 centimetres) on December 11 and peaking on December 12, Buffalo and Rochester in western New York received 13.6 and 22.3 inches (35 and 57 centimetres) of snow, respectively, from the storm, while Syracuse received 18.2 inches (46 cm) over three days commencing December 12. [81] [82] The Mayors of Buffalo and Rochester declared States of Emergency and schools, universities, department stores, restaurants, and most public buildings were closed on December 12 in both cities. [12] [83] [84] Most war production plants and other larger factories in all three cities were closed for at least a day as well. [12] Rail transport and intercity bus service through central New York to Syracuse, Rochester, Buffalo and areas further west was at a standstill on December 12 and 13 due to snow drifts from the storm. [12] [85]
Smaller cities, such as Jamestown in the southwest, with 26 inches (66 cm) over four days, Binghamton in the south-central area of the state with 12 inches (30 cm), and Watertown in the north of the state with 11 inches (28 cm), also received substantial snowfalls. New York City only had a sprinking of snow and high winds, which did result in most flights being cancelled. [12] Eleven people died in New York State from the snowstorm—some due to heart attacks from the exhaustion of shovelling or walking in snow, some from vehicular accidents, including as pedestrians, and also an expectant mother and her baby after the mother spent eight hours struggling to get to the Lockport Hospital, during which time an amubulance carrying her got trapped in a snow drift and the first municipal plow sent to extricate the ambulance broke down. [23] [86] [87] [88]
Aside from the now-closed grade-separated Rochester Subway, transportation in Rochester was completely paralyzed by the 22 inch-plus snowfall—"hundreds of buses" were marooned all over the city and its suburbs; only one main bus route was somewhat operational of December 12; cars and trucks were immobile and mired in snow drifts everywhere; and, workers whose shifts were ending could not get home, and vice versa. [89] Some war plants, as well as the Eastman Kodak manufactory, kept some stranded workers working overtime and set up cots for them to sleep, but eventually they closed down for a day or more. [12] [89] The night of December 12, several hundred workers or shoppers who were stranded in downtown Rochester were accommodated by cots in hotel hallways or even the conversion of single hotel rooms to dormitory-style rooms. [89]
Power outages cut power to one war plant and to hundreds of homes and high voltage wires crossed lighting circuits burning out 1,600 street lights. [90] [91] Only 35% of the operators for the telephone company were able to get to work December 12 and, as telephone calls soared, operators were working long hours of overtime—on December 13 over one million calls were attempted (compared to 530,000 on a normal day) but only 715,000 could be put through. [89] [91] [92] The Rochester Democrat and Chronicle published a reduced number of newspapers for December 13 and stated it was unfeasible to disbritute them beyond downtown hotels and newsstands. [93] It also indicated that until the snow emergency was ameliorated, the paper would omit all advertising in order to reduce the weight of newspapers to be delivered. [93]
Thirty-four of the 41 independent contractors assigned by the city to clear snow declined to do so as the verbally-agreed-upon rate of pay was based on the distance plowed, not the amount of snow needing to be plowed or the amount of time required. [94] Accordingly, the removal of snow from roads and sidewalks was severely delayed, meaning private vehicle travel was extremely difficult and most bus routes were inoperational for several days, which led to the decision to close schools until after the Christmas Break and to most war plants only resuming normal production four days after the storm. [95]
To deliver emergency food and/or medicine to about 50 snow-bound homes, a group of ten people rode on horseback; they were also available to transport doctors to emergencies, if necessary. [96] Food deliveries could not be made to the stores and markets of the city, which were mostly downtown—on December 13 only 3 truckloads of milk of the usual 70 truckloads was able to be delivered to the city. [97] Only on December 15 was close to the usual daily amount of food finally able to be delivered, including the first vegetables and fruits, although the dairies pleaded for people "to dig up any bottles that might be buried in snow" as there was a shortage of milk bottles; with the then snow-blocked usual home delivery of milk, the delivery person picked up the used bottles. [98]
On December 14, Rochester requested assistance from surrounding municipalities and from the New York State Governor—the state provided 20 heavy-duty plows that were finished plowing state highways and roads in their respective areas; the arrival of heavy-plows was fortitious as colder weather the evening of December 15 made the snow harder-packed, almost ice-like, which required heavy-duty plows. [95] [99] By December 16, about nine of the city's 15 bus routes were finally operating, on December 17, 80% of city streets had been plowed to some extent and all city bus routes were operating, although some suburban routes were still suspended, and on December 18, the airport finally reopened as snow plows were available to clear the runways. [95] [100]
Most of Southern Ontario, received 20 cm (7.9 in) or more of snow which, after being blown into snow drifts by substantial winds, blocked most highways, leaving most cities, towns and hamlets isolated for up to a day or more. [101] [102] Within most cities and towns, local car travel and transit was mostly impossible as well, and for most, intercity bus travel did not resume for at least two days because highways were initially only plowed a minimal width. [103] [104] [102] [101] In southwestern Ontario, where snowfall began late on December 10 or early on December 11, accumulations included 22.3 cm (8.8 in) in Windsor, 25.6 cm (10.1 in) in London, and 20.3 cm (8.0 in) in Kitchener. [105] [106] [107] In eastern Ontario, snowfall accumulations included 35.5 cm (14.0 in) in Peterborough, 31.0 cm (12.2 in) in Kingston, and 20.1 cm (7.9 in) in Ottawa. [108] [109] [110] Areas along Lake Huron and Georgian Bay received minimal snow, with Owen Sound, situated in-between those two bodies of water, recording 8.4 cm (3.3 in), although Orillia in Central Ontario to the east of Georgian Bay, received 31.0 cm (12.2 in). [111] [112] [113]
The Orangeville-Georgetown area received 40.3 cm (15.9 in) of snow and hundreds of people in rural areas near there were stranded without power or telephone service for days until the roads could be cleared. [114] [115] In Woodstock, located on Highway 2, the main highway between London and Toronto, 100 trucks were stalled in snow or waiting within the city for the highway to be cleared on December 12. [111] [101] [116] West of London, a convoy of 25 US army trucks, mostly driven by women, were stuck in snow drifts for several hours on December 12. [117] Most of Ontario's main highways (Highways 2, 3, 5, 6, 7, 8 and the Queen Elizabeth Way) were all open to at least car-widths by December 14 as 100 airmen from the Royal Canadian Air Force operated the Force's plows along those routes beginning late December 12. [118] However, the Department of Highways still advised on December 14 it considered the highways open only to essential traffic as snowpiles/banks right next to the edge of driving lanes needed to be pushed back. [118] [119]
Ottawa was not significantly impacted by the storm as milk deliveries continued, streetcar service operated mostly on schedule and roads were all plowed by the morning of December 13, although intercity bus service was paused until late December 13. [120] At least 21 fatalities occurred in Ontario due to the storm—aside from multiple fatalities in Toronto and Hamilton, single fatalities occurred in Oshawa, Brantford, Campbellford, Woodstock and Richmond Hill, most from heart attacks from exhaustion. [102] [26]
Beginning with flurries on December 11, and intensifying after midnight and ending that afternoon, the Great Snowstorm deposited 57.2 cm (22.5 in) of snow on Toronto, which is still the second most in the city's history (behind 58.5 cm in 1872). [lower-alpha 2] [122] [123] [124] [125] The 48.3 cm (19.0 in) of snow on December 12 remains the single-day record for the city. [123] [126] Winds of at least 50 km/h (30 m/ph) piled many drifts as high as 3 metres (9.8 feet), trapping some people in their homes. [122] [124] [127] On December 12, moving around the city was almost impossible and all schools, the University of Toronto, the Toronto Stock Exchange, courts, department stores and 80% of other stores and businesses never opened that day. [111] [101] [128] [124] The Toronto Daily Star published limited copies for December 12 and The Globe and Mail cancelled its December 13 paper. [123] [116] Only the Yonge, King and Queen lines of Toronto's 15 streetcars lines were able to be kept open all day, but only at a reduced and slower service level, as every section that was cleared was soon refilled by both drifting and newly-fallen snow. [122] [129] [130] Bus service was suspended and commuter train lines were mostly blocked, leaving people in suburbs, such as Weston, Leaside and Long Branch, isolated. [131] [111] [lower-alpha 3]
Numerous war production factories and other industries did not operate because only a small percentage workers could get to them; in most cases they did not restart operations until the late afternoon shift on December 13 or the morning of December 14. [123] [129] [132] Workers ending their night shifts could not get home; 200 workers at Victory Aircraft in Malton in four buses and numerous private cars were stranded for over 12 hours in the hamlet of Woodhill as Highway 7 to Brampton where they lived was totally blocked by 2-metre (6.6-foot) snow drifts. [111] [133] [134] They slept in a school and two service stations with food in the hamlet's stores nearing depletion. [133] Workers at the oil refinery in Port Credit, as well as six buses and several transport trucks, were marooned by snow drifts for over 24 hours. [135]
The Mayor directed people to stay home unless their jobs were essential, [111] [101] [136] while the Province issued an order banning all non-essential vehicles from any streets in Toronto with streetcar tracks, that being most of the main roads. [123] [129] The blocked roads to and within the rural areas around Toronto prevented almost all milk, other food and coal from being delivered to the city on December 12; only 3% of the usual milk supply arrived. [5] [123] The Mayor, the evening of December 12, broadcast on the radio a request that people restrict bread and milk consumption and the City transported emergency food to fire halls the next day, from where residents could make purchases if stores were inaccessible. [123] [137] [125] By December 14, the city was arranging for emergency coal distribution to 26 fire halls as households without coal were unable to heat their homes or cook food. [138] [139] [134] Milk deliveries from farmers could not increase to approaching normal levels until December 14 and even then the supply was endangered for a few additional days on account of an acute shortage (100,000) of milk bottles, prompting the Toronto Milk Producer's Association to issue a plea for residents to return any bottles they had. [140] [141] [138] [134]
By late evening of December 12, the roads and tracks had been cleared to permit 12 of Toronto's 15 streetcar lines to operate, although with less cars than usual as 70 drivers were still needed to clear snow. [142] [lower-alpha 4] On the morning of December 14, most suburban bus and commuter train lines were finally operating and schools, many stores and businesses reopened. [26] [129] Only on December 16 were most of the city's 920 km (570 mi) of roads passable—that meant one-lane's width cleared. [141]
Between 13 and 16 people died in Toronto, most from heart attacks from struggling through deep snow and two from heart attacks while shovelling. [26] [143] [144] [5] One person died when a streetcar turned on its side, with 43 passengers suffering injuries, 10 seriously. [145] [5] An estimated 100 people were seriously injured in Toronto from falls and other accidents caused by the storm, with at least 54 of those being fractures. [35] [102] Hospitals were overflowing and ambulances were incapable of making trips due to the deep snow. [101] [lower-alpha 5] Transportation into Toronto was greatly hindered: the airport had no flights for over 36 hours; [26] trains were delayed by up to ten hours on December 12 and 13 due to electrical switches in the multi-track junctions near Toronto being smothered with ice and snow; [147] [116] and, no intercity buses ran until late on December 13. [123] [143]
The highest snowfalls in Ontario were in Hamilton with 62.5 cm (24.6 in) and St. Catharines with 66 cm (26 in). [6] [148] [149] The storm caused the complete curtailment of streetcar and bus service in Hamilton for over a day and only minimal service being available for an additional day. [150] [151] One neighbourhood, population 10,000, was only reached by plows the morning of December 14 after two nights of isolation without any deliveries of food or coal. [6] [102] McMaster University was closed for two days, public schools were closed three days, most milk or bread deliveries did not occur for three days, and it took five days for all transit operations, including suburban buses, to return to regular service. [148] [6] The QEW and other highways from Hamilton to the rest of the Niagara Peninsula were blocked with snow for almost two days—the QEW had 3 and 3.5-metres (10 and 12 feet) of snow in some valley areas. [149] [150] [152] All bus or street railway service within and between urban areas in eastern Niagara was suspended for up to two days; this prompted people to utilize horse-drawn sleighs to get around, including by the St. Catharines Standard to deliver its newspapers. [153] [149] In Welland, which received 43.2 cm (17.0 in) of snow, 1,000 workers at the Welland Chemical Works were stranded at the plant overnight until a bulldozer cleared the access road. [154] [118] There were three fatalities in the region, all in Hamilton. [26] [117]
Montreal received 29.9 cm (11.8 in) of snow, mostly on December 12, accompanied by 48 m/ph (77 km/h) gales, but it had staff of 1,500 men and more than 620 pieces of equipment ready to work in 12-hour shifts to clear snow, so the storm did not substantially impact the city even though it was still recovering from a 41.9 cm (16.5 in) snowfall earlier in the month. [155] [156] [157] Streetcar transit had no substantial disruptions other than drivers having to drive slowly due to poor visibility from the snow/wind combination. [157] Flights were grounded for 24 hours but train service remained normal aside from trains from Toronto, which were delayed four to ten hours on December 12 and 13. [158] [156] Other cities in Quebec received lighter amounts of snow on December 12 and 13—Quebec City 6.4 cm (2.5 in), Sherbrooke 8.4 cm (3.3 in) and Chicoutimi 8.7 cm (3.4 in). [159] [160] [161]
A blizzard is a severe snowstorm characterized by strong sustained winds and low visibility, lasting for a prolonged period of time—typically at least three or four hours. A ground blizzard is a weather condition where snow is not falling but loose snow on the ground is lifted and blown by strong winds. Blizzards can have an immense size and usually stretch to hundreds or thousands of kilometres.
The North American blizzard of 1996 was a severe nor'easter that paralyzed the United States East Coast with up to 4 feet (1.2 m) of wind-driven snow from January 6 to January 8, 1996. The City University of New York reported that the storm "dropped 20 inches of snow, had wind gusts of 50 mph and snow drifts up to 8 feet high." This storm was a classic example of a nor'easter, but the storm would not have been as historically significant without the presence of the arctic high pressure system located to the north of New York. It was followed by another storm, an Alberta Clipper, on January 12, then unusually warm weather and torrential rain which caused rapid melting and river flooding in the Northeast Floods later that month. Along with the March Superstorm of 1993 and the January 2016 United States blizzard, it is one of only three snowstorms to receive the top rating of 5, or "Extreme", on the Northeast Snowfall Impact Scale (NESIS).
The Blizzard of 1999 was a strong winter snowstorm which struck the Midwestern United States and portions of central and eastern Canada, hitting hardest in Iowa, Wisconsin, Illinois, Indiana, Michigan, Ohio, southern Ontario, and southern Quebec dumping as much as 60 centimetres (2 ft) of snow in many areas. Chicago received a recorded 21.6 in (55 cm). The storm hit just after New Year's Day, between January 2 and January 4, 1999. Travel was severely disrupted throughout the areas and the cities of Chicago and Toronto were also paralyzed. Additionally, record low temperatures were measured in many towns in the days immediately after the storm.
The February 2007 North American blizzard was a massive winter storm that affected most of the eastern half of North America, starting on February 12, 2007 and peaking on Valentine's Day, February 14. The storm produced heavy snowfalls across the midwestern United States from Nebraska to Ohio and produced similar conditions across parts of the northeastern United States, and into Canada in Ontario, Quebec and New Brunswick. Significant sleet and freezing rain fell across the southern Ohio Valley and affected portions of the east coast of the United States, including the cities of Boston, Baltimore, Washington, D.C., New York City and Philadelphia.
The Mid-December 2007 North American winter storms were a series of two winter storms that affected much of central and eastern North America, from December 8 to December 18, 2007. The systems affected areas from Oklahoma to Newfoundland and Labrador with freezing rain, thunderstorms, sleet, snow, damaging winds, and blizzard-like conditions in various areas. The first two storms produced copious amounts of ice across the Midwestern United States and Great Plains from December 8 to December 11, knocking out power to approximately 1.5 million customers from Oklahoma north to Iowa. The second storm moved northeast, producing heavy snow across New York and New England. A third storm was responsible for a major winter storm from Kansas to the Canadian Maritimes, bringing locally record-breaking snowfalls to Ontario, an icestorm across the Appalachians, and thunderstorms and 9 tornadoes to the Southeastern United States.
The North American blizzard of 2008 was a winter storm that struck most of southern and eastern North America from March 6 to March 10, 2008. The storm was most notable for a major winter storm event from Arkansas to Quebec. It also produced severe weather across the east coast of the United States with heavy rain, damaging winds and tornadoes, causing locally significant damage. The hardest hit areas by the wintry weather were from the Ohio Valley to southern Quebec where up to a half a meter of snow fell locally including the major cities of Columbus, Ohio, Cleveland, Ohio, and Ottawa, Ontario. For many areas across portions of the central United States, Ontario and Quebec, it was the worst winter storm in the past several years. The blizzard and its aftermath caused at least 17 deaths across four US states and three Canadian provinces, while hundreds others were injured mostly in weather-related accidents and tornadoes.
The Chicago blizzard of 1979 was a major blizzard that affected northern Illinois and northwest Indiana on January 13–14, 1979. It was one of the largest Chicago snowstorms in history at the time, with 21 inches (53 cm) of snowfall in the two-day period. Only 2 inches (5.1 cm) to 4 inches (10 cm) of snow was expected but by the end of Sunday, January 14, the depth of snow on the ground peaked at 29 inches (74 cm). The blizzard lasted for a total of 38 hours. At its peak, wind gusts reached speeds of 39 miles (63 km) per hour. Five people died during the blizzard, with approximately 15 others seriously injured due to conditions created by the storm. One of the five deaths came when a snowplow driver went berserk, hitting 34 cars and ramming a man.
The North American blizzard of 1947 was a record-breaking snowfall that began without prediction on Christmas and brought the northeastern United States to a standstill. The snowstorm was described as the worst blizzard in the region after that of 1888. The storm was not accompanied by high winds, but the snow fell silently and steadily. By the time it stopped on December 26, accumulation had reached 26.4 inches in Central Park in Manhattan. Similar or greater accumulations were noted in all of metropolitan New York and New Jersey, as well as in upstate New York, Connecticut, and most of the mid-Atlantic region.
The December 1960 nor'easter was a significant early-season winter storm that impacted the Mid-Atlantic and New England regions of the United States. Moderate to heavy snowfall fell from West Virginia to eastern Maine, amounting to 10 in (25 cm) or more in parts of 13 states and peaking at 21.4 in (54 cm) at Newark, New Jersey. The storm was accompanied by strong winds, gusting to over 90 mph (140 km/h) in coastal New England, and left in its wake a dangerously cold air mass. The storm originated in a weak low pressure area which formed over the western Gulf of Mexico on December 10. A secondary low developed over South Carolina on the next day, supported by the merger of two troughs aloft. Sliding southeast of New England, the new storm explosively deepened to become a full-fledged nor'easter, with a minimum central air pressure of 966 mbar. It began to weaken over the Canadian Maritimes.
Global storm activity of 2008 profiles the major worldwide storms, including blizzards, ice storms, and other winter events, from January 1, 2008, to December 31, 2008. A winter storm is an event in which the dominant varieties of precipitation are forms that only occur at cold temperatures, such as snow or sleet, or a rainstorm where ground temperatures are cold enough to allow ice to form. It may be marked by strong wind, thunder and lightning, heavy precipitation, such as ice, or wind transporting some substance through the atmosphere. Major dust storms, Hurricanes, cyclones, tornados, gales, flooding and rainstorms are also caused by such phenomena to a lesser or greater existent.
The December 2010 North American blizzard was a major nor'easter and historic blizzard affecting the Contiguous United States and portions of Canada from December 22–29, 2010. From January 4–15, the system was known as Windstorm Benjamin in Europe. It was the first significant winter storm of the 2010–11 North American winter storm season and the fifth North American blizzard of 2010. The storm system affected the northeast megalopolis, which includes major cities such as Norfolk, Pittsburgh, Philadelphia, Newark, New York City, Hartford, Providence, and Boston. It brought between 12 and 32 inches of snow in many of these areas.
The Chicago blizzard of 1967 struck northeast Illinois and northwest Indiana on January 26–27, 1967, with a record-setting 23 inches (58 cm) snow fall in Chicago and its suburbs before the storm abated the next morning. As of 2024, it remains the greatest snowfall in one storm in Chicago history. As the blizzard was a surprise during the day with people already at work or school, it stopped the city for a few days as people dug out. "The storm was a full-blown blizzard, with 50 mph-plus northeast wind gusts creating drifts as high as 15 feet."
The January 31 – February 2, 2015 North American blizzard was a major winter storm that plowed through the majority of the United States, dumping as much as 2 feet (24 in) of new snowfall across a path from Iowa to New England, as well as blizzard conditions in early February 2015. It came less than a week after another crippling blizzard which impacted the Northeast with 2–3 feet of snow. It was the first of many intense winter storms to occur in the nation during the month of February, partly in due to an ongoing cold wave that was beginning to take shape shortly after the storm subsided.
The 2018–19 North American winter was unusually cold within the Northern United States, with frigid temperatures being recorded within the middle of the season. Several notable events occurred, such as a rare snow in the Southeast in December, a strong cold wave and several major winter storms in the Midwest, and upper Northeast and much of Canada in late January and early February, record snowstorms in the Southwest in late February, deadly tornado outbreaks in the Southeast and a historic mid-April blizzard in the Midwest, but the most notable event of the winter was a record-breaking bomb cyclone that affected much of the Central United States and Canada in mid-March. Unlike previous winters, a developing weak El Niño was expected to influence weather patterns across North America. Overall, however, winter of 2018–19 had many La Niña like conditions, being mild along the mid- and lower parts of the East Coast, the West Coast, and most of the southern Plains. Overall, the meteorological winter of 2018-19 became the wettest on record for the United States.
The 2019–20 North American winter was unusually warm for many parts of the United States; in many areas, neutral ENSO conditions controlled the weather patterns, resulting in strong El Niño like conditions and the sixth-warmest winter on record, and many areas in the Northeastern United States saw one of the least snowy winters in years. In fact, Baltimore and Islip saw no snow in February for the first time. Some notable events still occurred, such as a powerful blizzard that impacted the Western United States in late November, a series of cold shots in January and February, a snowstorm within the Texas Panhandle and a late-season blizzard in the High Plains.
The December 15–17, 2020 nor'easter was a powerful nor'easter that hammered the Northeastern United States and produced widespread swaths of over 1 foot (12 in) of snow in much of the region from December 15–17, 2020, ending a 1,000+ day high-impact snowstorm drought in much of the Mid-Atlantic and coastal New England regions. The system developed out of a weak area of low-pressure that first developed over the Central United States producing some snowfall before moving eastward, and by December 16, a new, dominant area of low pressure began to develop along the Southeast coast. This low steadily deepened as it moved along and impacted the Mid-Atlantic coastline, prompting several winter-related advisories and warnings for much of the Northeast.
The January 14–17, 2022 North American winter storm brought widespread impacts and wintry precipitation across large sections of eastern North America and parts of Canada. Forming out of a shortwave trough on January 13, it first produced a swath of snowfall extending from the High Plains to the Midwestern United States. The storm eventually pivoted east and impacted much of the Southern United States from January 15–16 before shifting north into Central Canada, the Mid-Atlantic states, and the Northeastern United States. The system, named Winter Storm Izzy by The Weather Channel, was described as a "Saskatchewan Screamer".
The Great Lakes Blizzard of January 1971 affected almost the entire Great Lakes region of North America, as well as the western St. Lawrence Valley and northern New England between January 25 and 28, 1971 before a second severe snowstorm hit many of the same areas between January 28 and 31, 1971. The areas that felt the fiercest effects of the dual storms, that being moderate or heavy snow, sustained high winds, and zero visibility due to blowing snow, included southern Wisconsin, most of Michigan, Southern Ontario, northeastern Ohio, northwestern Pennsylvania, most of upstate New York and Southern Quebec, while northern Wisconsin, northern Indiana, northeastern Ontario, and northern Vermont experienced blizzard conditions from the first of the storms.
The 2022–23 North American winter was an unusually warm winter for the east and an unusually cold winter for the west in North America, as it occurred across the continent from late 2022 to early 2023. The winter season in North America began at the winter solstice, which occurred on December 21, 2022, and it ended at the March equinox, which occurred on March 20, 2023. The first day of meteorological winter began on December 1 and unofficially ended on February 28; winter storms may still occur outside of these limits.
In November 2022, a severe lake-effect winter storm impacted parts of Pennsylvania, Ohio, and New York, causing high accumulations of snow across the Great Lakes region, including snowfall accumulations upwards of 50 in (130 cm) in several locations. In Hamburg, New York, 81.2 in (206 cm) fell, while Orchard Park, New York recorded 80 in (200 cm) of snow. At least four fatalities occurred, with three in New York and one in Indiana, and several highways closed after heavy snowfall. A travel ban was also issued for New York by governor Kathy Hochul, and thundersnow occurred across areas impacted by the winter storm.
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