|Storm type:||Cyclonic blizzard, Nor'easter|
|Formed:||March 11, 1993|
|Dissipated:||March 15, 1993|
|60 inches (152.4 cm) - Mt. Le Conte, TN|
|960 mbar (hPa)|
|Damages:||$6.65-11 billion (2009 USD)|
|Areas affected:||Canada, North America, and Central America|
^* Maximum snowfall or ice accretion
The Storm of the Century, also known as the ’93 Superstorm, No-Name Hurricane , the White Hurricane, or the (Great) Blizzard of 1993, was a large cyclonic storm that occurred on March 12–March 13, 1993, on the East Coast of North America. It is unique for its intensity, massive size and wide-reaching effect. At its height the storm stretched from Canada to Central America, but its main impact was on the Eastern United States and Cuba. Areas as far south as central Alabama and Georgia received 6 to 8 inches (20 cm) of snow and areas such as Birmingham, Alabama, received up to 12 inches (30 cm) with isolated reports of 16 inches (41 cm). Even the Florida Panhandle reported up to 4 inches (10 cm), with hurricane-force wind gusts and record low barometric pressures. Between Louisiana and Cuba, hurricane-force winds produced high storm surges in the Gulf of Mexico, which along with scattered tornadoes killed dozens of people.
A "disorganized area of low pressure" that formed in the Gulf of Mexico joined an arctic high pressure system in the Midwestern Great Plains, brought into the mid-latitudes by an unusually steep southward jet stream. These factors combined to produce unusually low temperatures across the eastern half of the United States.
The 1993 Storm of the Century marked a milestone in U.S. weather forecasting. By March 8 (and by some accounts even earlier), several operational numerical weather prediction models and medium-range forecasters at the US National Weather Service recognized the threat of a significant snowstorm. By the 12th, many had reviewed the data and were convinced that a serious threat loomed overhead. This marked the first time that National Weather Service meteorologists were able to accurately predict a system's severity five days in advance. Official blizzard warnings were issued two days before the storm arrived, as shorter-range models began to confirm the predictions. Forecasters were finally confident enough in the computer-forecast models to support decisions by several Northeastern U.S. states to declare a State of Emergency before the snow even started to fall.
In the South, however, temperatures in the days prior to the storm were typical for early March. Although large fluctuations in temperature are not unusual in the deep south, many residents doubted that freezing temperatures could return so rapidly; nor that snow was likely due to the rarity of significant snowfall later than February. Many local TV news stations were reluctant to even broadcast the forecast models, due to the extreme numbers being predicted by the computers, but the models turned out to be right.
During Friday March 12, temperatures over much of the eastern United States began to fall quickly. The area of low pressure rapidly intensified during the day on Friday and moved into northwest Florida by early Saturday morning. As this happened snow began to spread over the eastern United States, and a large squall line moved from over the Gulf of Mexico into Florida and Cuba. The low tracked up the east coast during the day on Saturday and into Canada by early Monday morning.
Temperatures accompanying the storm were unseasonably cold for late winter so close to spring: average daily maximum temperatures, in mid-March, are around 46°F (8°C) in Boston, 51°F (11°C) in Philadelphia, and 65°F (18°C) in Atlanta. During the 1993 storm, these places were all near or below freezing, and parts of New England saw daily maximum temperatures as low as 14°F (-10°C). Record low temperatures for March were recorded in much of the Southern U.S.
This storm complex was massive, affecting at least 26 U.S. states and much of eastern Canada. Bringing cold air along with heavy precipitation and hurricane force winds, it caused a blizzard over much of the area it affected, including Thundersnow from Texas to Pennsylvania and widespread whiteout conditions. Snow fell as far south and east as Jacksonville, Florida, and areas of the Florida Panhandle got several inches of snow, making it the biggest winter storm to affect the state since 1899. Ice pellets (sleet) mixed in with the rain as temperatures in Tampa hovered in the lower 40's after frontal passage.
Some affected areas in the Appalachian region saw more than 3.5 feet (1.1 m) of snow, and snowdrifts were as high as 35 feet (10.7 m). Responsible for 300 deaths and the loss of electric power to over 10 million, it is purported to have been directly experienced by over 130 million people in the United States, about half the country's population at that time. Every airport from Halifax, Nova Scotia to Atlanta, Georgia was closed for some time because of the storm. The volume of the storm's total snowfall was later computed to be 12.91 mi³ (53.96 km³), an amount which would weigh (depending on the variable density of snow) between 5.4 and 27 billion tonnes.
Barometric pressures recorded during the storm were also unusually low: readings of 28.35 inHg (960 mb or hPa) were observed in New England. Usually, such low readings are observed only in hurricanes (generally of Category 2 or 3 intensity on the Saffir-Simpson hurricane scale), which peak at almost the exact opposite time of year, or in other cyclonic storms far out to sea. It also pushed a storm surge ashore on the Florida panhandle, drowning a few people taken by surprise at the storm's ferocity.
As one of the most powerful storms in recent history, the storm has been described as the "Storm of the Century" by many of the areas affected. The last blizzard to have such an effect on the Southeast was the Great Blizzard of 1899.
Besides producing record low barometric pressure across a swath of the Southeast and Mid-Atlantic states, and one of the nation's biggest snowstorms, the low produced a potent squall line ahead of its cold front. The squall line produced a serial derecho as it moved into Florida and Cuba around midnight on March 13. Straight-line winds gusted above 100 mph/85 kts (160 km/h) at many locations in Florida as the squall line moved through.
A substantial storm surge was also generated along the gulf coast from Apalachee Bay in the Florida panhandle to south of Tampa Bay. Due to the angle of the coast relative to the approaching squall, Taylor County along the eastern portion of Apalachee Bay and Hernando County north of Tampa were especially hard hit.
Storm surges in those areas reached up to 12 feet (3.7 m); higher than many hurricanes. With little advanced warning of incoming severe conditions, some coastal residents were awakened in the early morning of March 13 by the waters of the Gulf of Mexico rushing into their homes. Overall, the storm's surge, winds, and tornadoes damaged or destroyed 18,000 homes and killed at least 12 people in Florida.
In Cuba, wind gusts reached 100 mph (160 km/h) in the Havana area. A survey conducted by a research team from the Institute of Meteorology of Cuba suggests that the maximum winds could have been as high as 130 mph (210 km/h). It is the most damaging squall line ever recorded in Cuba.
There was widespread and significant damage in Cuba, with damages estimated as intense as F2. The squall line finally moved out of Cuba near sunrise, leaving 10 deaths and US$1 billion in damage on the island.
The storm also had a substantial impact on Central America and parts of Asia. In Belize, many local communities believed the primary squall line was actually artillery fire from the country's western border with Guatemala. Nearly all communities in Belize lost electricity and many roofs were blown off houses. It took months to clear away the debris and fallen trees from remote areas and forested roads. Offshore barrier islands also had unusual damage on their west facing coastlines from the storm surge and high winds. Damage amounts and fatality reports have never been tallied or confirmed, as most citizens of Belize never fully understood that this superstorm stretched all the way to Canada.
In the image above, measured gusts in mph are plotted (blue numbers). "+" symbols indicate the locations of wind damage or estimated wind gusts above severe limits (58 mph or greater). Red dots and paths indicate tornado events. Small red numbers indicate tornado intensities in F-scale. The approximate location of the squall line "gust front" is shown in two hour increments (curved purple lines).
|F#||Location||County||Time (UTC)||Path length||Damage|
|F2||NW of Chiefland||Levy||0438||1 miles (1.6 km)||3 deaths|
|F1||E of Crystal River||Citrus||0438||0.5 miles (0.8 km)|
|F0||Treasure Island area||Pinellas||0500||0.1 miles (0.16 km)|
|F0||New Port Richey area||Pasco||0504||0.1 miles (0.16 km)|
|F2||Ocala area||Marion||0520||15 miles (24 km)|
|F1||N of La Crosse||Alachua||0520||0.8 miles (1.3 km)||1 death|
|F2||NW of Howey Height to Alamonte Springs||Lake||0530||30 miles (48 km)||1 death|
|F0||Tampa area||Hillsborough||0530||0.1 miles (0.16 km)|
|F1||Jacksonville area (1st tornado)||Duval||0600||0.8 miles (1.3 km)|
|F0||Bartow area||Polk||0600||0.1 miles (0.16 km)|
|F0||Jacksonville area (2nd tornado)||Duval||0610||0.1 miles (0.16 km)|
In the South, where public works facilities (in most areas) generally have no reason to be prepared for snow removal, the storm is vividly remembered because it resulted in a complete shutdown of that region for three days. Cities that usually receive little snowfall, such as Chattanooga, Tennessee, received anywhere from 2 to 4 feet (1.2 m) of snow, causing some municipalities to adopt at least an emergency winter-weather plan for the future where one might not have existed before. Birmingham, Alabama, which normally receives 1-inch (2.5 cm) in a year, received 17 inches (43 cm) shattering the records for most snow in a single storm, a single month, and even a single season. The psychological impact in the Southern states, where average high temperatures in March tend to run into the 60s Fahrenheit (the upper teens Celsius), was magnified by the fact that it struck a week before spring. Two NASCAR weekends—one at Atlanta Motor Speedway, where the Motorcraft 500 Winston Cup round was postponed six days, and the Slick 50 300 Busch Grand National Series event was postponed eight months, and the Miller 500 Classic weekend for the Busch Grand National cars and Late Models at Martinsville Speedway was postponed two months because of the aftereffects of the soggy grounds—were called off because of the weather and its ensuing rain; Birmingham recorded a record low of 2 °F (−17 °C) during the storm. Syracuse, New York, which is accustomed to heavy snowfall due to yearly lake-effect snow storms, received a record 43 inches (110 cm) from the storm, while snowfall totaled over 12 inches (30 cm) in New York City and 2 feet (0.61 m) of snow fell in Hartford, Connecticut and Pittsburgh, Pennsylvania.
The weight of record snows collapsed many factory roofs in the South, and snowdrifts on the windward sides of buildings caused a few decks with substandard anchors to fall from homes. Though the storm was forecast to strike the snow-prone Appalachian Mountains, hundreds of people were nonetheless rescued from the Appalachians, many caught completely off-guard on the Appalachian Trail, or visiting cabins and lodges in remote locales. Drifts up to 14 feet (4.3 m) were observed at Mount Mitchell. Snowfall totals of between 2 and 3 feet (0.91 m) were widespread across northwestern North Carolina. Boone, North Carolina — in a high-elevation area accustomed to heavy snowfalls — was nonetheless caught off guard by 24 hours of below zero Fahrenheit temperatures along with storm winds, which (according to NCDC storm summaries) gusted as high as 110 miles per hour. Electricity was not restored to many isolated rural areas for a week or more, with power cuts occurring all over the east. Nearly 60,000 lightning strikes were recorded as the storm swept over the country, for a total of seventy-two hours, and many may remember their local news organizations touting the term "thundersnow."
Overall, the blizzard of 1993 caused a total of $6.6 billion of damage.
Across the Northeastern states and eastern Canadian provinces, the storm put down an average of 15 inches (40 cm) of snow, which, though most certainly heavy, is not exceptional by most local standards, but still somewhat unusual for mid-March, especially for the southernmost parts of the region such as the Baltimore-Washington area. In southeastern Ontario and southwestern Quebec where less severe winter blizzards are relatively common the 15 inch/40 cm+ amounts received in Montreal and Ottawa were nevertheless far above average and came only second to record amounts set during the deadly Eastern Canadian Blizzard of March 1971, an exceptionally brutal Nor'easter still locally referred to in Quebec and parts of NY State as the "Storm of the Century". For their part New England residents tend to point to the Blizzard of 1978 as their "storm of the century," due largely to its unrelenting snowfall, which temporarily dislocated the weather-hardened region, while Mid-Atlantic residents tend to point to the Blizzard of 1996 for similar reasons. Based on widespread effects, barometric pressures, wind speeds and satellite images, however, there is little doubt that the storm of 1993 was the most remarkable overall. It may have been the largest one-piece storm in recorded history.
Totals are for the main system only.
|Mount Le Conte, TN||60 in (152.4 cm)|
|Mount Mitchell, NC||50 in (127 cm)|
|Snowshoe, WV||44 in (111.8 cm)|
|Syracuse, NY||43 in (109.2 cm)|
|Latrobe, PA||36 in (91.4 cm)|
|Lincoln, NH||35 in (88.9 cm)|
|Boone, North Carolina||33 in (83.8 cm)|
|Gatlinburg, TN||30 in (76.2 cm)|
|Albany, NY||27 in (68.6 cm)|
|Pittsburgh, PA||25 in (63.5 cm)|
|Hartford, CT||24 in (60.9 cm)|
|London, KY||22 in (55.9 cm)|
|Worcester, MA||20.1 in (51.0 cm))|
|Chattanooga, TN||20 in (50.8 cm)|
|Asheville, NC||19 in (48.2 cm)|
|Ottawa, ON||17.7 in (45 cm)|
|Birmingham, AL||17 in (43 cm)|
|Montreal, QC||16.1 in (41 cm)|
|Washington, D.C. (Dulles)||14.1 in (36 cm)|
|New York, NY (LaGuardia)||12.3 in (31 cm)|
|New York, NY (Central Park)||10.6 in (27 cm)|
|New York, NY (Kennedy)||9.3 in (24 cm)|
|Washington, D.C. (Reagan)||6.6 in (17 cm)|
|Atlanta, GA||4 in (10 cm)|
|Mobile, AL||3 in (7.6 cm)|
|Hammond, LA||2 in (5.1 cm)|