1953 Worcester tornado

The 1953 Worcester tornado was an extremely powerful and destructive tornado that struck the city of Worcester, Massachusetts and surrounding areas on Tuesday, June 9, 1953, the final day of the Flint–Worcester tornado outbreak sequence. It stayed on the ground for 48 miles (77 km) and 78 minutes. The tornado injured 1,288 people and killed 94, making it one of the deadliest tornadoes in U.S. history[1] and the deadliest tornado to ever strike New England.[3] A total of 4,000 buildings were damaged or destroyed and, per National Weather Service estimates, 10,000 people were left homeless. The tornado caused $52.193 million (or $590 million [2023 USD] when adjusted for inflation) which, at the time, was the costliest tornado ever recorded.

"Worcester tornado" redirects here. For the baseball team, see Worcester Tornadoes.
1953 Worcester tornado
F4 tornado
Damage at Assumption College in Worcester
FormedJune 9, 1953, 4:25 p.m. EDT (UTC−04:00)
Duration1 hour and 18 minutes
DissipatedJune 9, 1953, 5:43 p.m. (UTC−04:00)
Max. rating1F4 tornado
Fatalities94 fatalities, 1,288 injuries[1][2]
Damage$52.193 million (1953 USD)[nb 1]
Areas affectedWorcester County in Massachusetts, principally in and near Worcester, Shrewsbury, Southborough, and Westborough

1Most severe tornado damage; see Fujita scale

At approximately 4:25 p.m. EST, the tornado developed in a forest near the town of Petersham, and proceeded to move through Barre, where two people were killed.[4] It then moved through the western suburbs of Worcester, where 11 more people were killed. The storm then passed through Worcester, where it destroyed Assumption College and several other buildings, killing 60. After striking Worcester, it killed 21 more people in the towns of Shrewsbury, Southborough, and Westborough, before dissipating over Framingham.

Meteorological synopsis

Buildup to storm
Surface weather analysis of the New England Region, June 9, 1953.

On June 7, 1953, a strong shortwave trough moved eastward over the Rocky Mountains, bringing with it strong upward motion that induced lee cyclogenesis: the formation of a low-pressure area over eastern Colorado. In combination with the warm unstable air in place over the Great Plains, and an elevated mixed layer from the desert southwest, this led to conditions favorable for severe thunderstorms and tornadoes.[5] More than 30 tornadoes occurred that day across Colorado, Kansas, Nebraska, and Iowa, including a violent tornado that killed 11 people near Arcadia, Nebraska.[6] On June 8 the storm system moved northeast [7] These conditions led to several tornadoes in the states of Michigan, Ohio, and Nebraska: most notably the Flint-Beecher tornado. The storm killed 116 people in the northern Flint suburb of Beecher, and injured 844. In addition, seven other tornadoes across the region caused 449 more injuries and 26 more fatalities. After the use of the Fujita scale began, the Flint-Beecher tornado was rated F5.[8]

On the morning of June 9, the low pressure system had moved northeastward into Ontario near the south end of Hudson Bay. An occluded front extended south from it, towards a triple point with a warm front and cold front near the northern end of Lake Superior. The warm front extended southeast across New York, Pennsylvania, and New Jersey, and over the course of the day moved northeast, bringing warm, moist, unstable air into the New England area, including Massachusetts. In the mid-atmosphere, the elevated mixed layer was still in place, keeping storms from forming earlier in the day before maximum temperatures were reached.[5] By afternoon, temperatures in Worcester had reached 80 °F (27 °C), with a dew point of 66 °F (19 °C); in combination with cold air aloft, this meant that atmospheric conditions were very unstable and conducive to severe weather. Along with this, amplified wind shear was present into the afternoon of June 9, which made conditions in the atmosphere supportive of supercell development, and the formation of tornadoes. [6]

Forecasters at the National Weather Service office in Boston believed that there was a possibility for tornado activity in the area; however, they did not include such an advisory in their forecast, fearing that people might panic unnecessarily.[9][5] 1953 was the first year that tornado and severe thunderstorm warnings were used, so forecasters compromised and issued the first severe thunderstorm watch in the history of Massachusetts.[9] Most news reports only made mentions of possible thunderstorms.[6] Because of this, the tornado struck with little to no warning for residents.[5][10]

Tornado event
F4 tornado damage from the Worcester tornado.

The tornado first developed over the Quabbin Reservoir in Petersham, Massachusetts at 4:25 p.m., and was witnessed by boaters on the reservoir - three funnels were seen at the beginning, with rapid dissipation of one of them. After brushing Petersham (occasionally with twin funnels several hundred feet apart), the tornado tracked southeastwards and slammed into the rural towns of Barre and Rutland, with two fatalities occurring at each of these locations.[11] The now massive tornado then tore directly through suburban Holden, completely wiping out the Brentwood Estates subdivision, resulting in fatalities.[12]

At 5:08 p.m., the tornado entered Worcester and grew to a width of one mile (1.6 km). The damage was phenomenal in Worcester (the second-largest city in Massachusetts) and in some areas equaled the worst damage in any U.S. tornado.[11] Hardest-hit areas included Assumption College (now home to Quinsigamond Community College), where a priest and two nuns were killed. The main building's three-foot (0.91 m)-thick brick walls were reduced by three floors, and the landmark tower lost three stories.[11] A nearby storage tank, weighing several tons, was lofted and tossed across a road by the tornado.[13] The nearby Burncoat Hill neighborhood saw heavy devastation (especially on its western slope), but it was the Uncatena-Great Brook Valley neighborhoods to the east of Burncoat Hill that were utterly leveled, with the tornado possibly reaching F5 intensity in this area.[11] Houses simply vanished, with the debris granulated and scattered well away from the foundations. Entire rows of homes were swept away in some areas. Forty people died in the Uncatena-Great Brook Valley areas alone. A 12-ton (10.89 metric-ton) bus was picked up, rolled over several times, and thrown against the newly constructed Curtis Apartments in Great Brook Valley, resulting in the deaths of two passengers. The Curtis Apartments blueprints were blown all the way to Duxbury (near Plymouth), 75 miles (121 km) away. Across Boylston St. from the Curtis Apartments, the Brookside Home Farm (a city-operated dairy facility and laundry) sustained total damage, with six men killed and the loss of its herd of 80 Holsteins. Houses and bodies were blown into Lake Quinsigamond. The six fatalities at Brookside were the most in any one building in the tornado's path.[12]

At approximately 5:20 p.m., the funnel moved into Shrewsbury, and maintained its one-mile (1.6 km) width throughout much of the town, killing 12. The tornado was still doing maximum damage when it moved through downtown Westborough (five deaths), where it began curving towards the northeast in its final leg. In the storm's final moments, three people perished in the collapse of the Fayville Post Office in Southborough.[12] Coincidentally, around the time it ended at 5:45 p.m., a tornado warning was issued, although by then it was too late. A separate F3 tornado also struck about the same time the warning was issued, in the nearby communities of Sutton, Northbridge, Mendon, Bellingham, Franklin, Wrentham and Mansfield in Massachusetts, injuring 17 persons. Another tornado did minor damage and caused several injuries in Fremont and Exeter in Rockingham County, New Hampshire; other smaller tornadoes occurred in Colrain, Massachusetts and Rollinsford, New Hampshire.

Baseball-size hail was reported in a score of communities affected by the Worcester supercell. Airborne debris was strewn eastward, reaching the Blue Hill Meteorological Observatory 35 miles (56 km) away, and even out over Massachusetts Bay and the Atlantic Ocean. The farthest documented distance of tornado debris was an item that blew from Holden to Eastham on Cape Cod, a distance of 110 miles (180 km). Some debris was found in the Atlantic Ocean. This is one of the greatest such instances in a U.S. tornado.[11]

Aftermath

The Worcester tornado's greatest effect on the nation was its being the principal catalyst for the Storm Prediction Center's reorganization on June 17, 1953, and subsequent implementation of a nationwide radar/storm spotter system. The results proved successful: only one tornado since the Worcester event - the EF5 tornado that struck Joplin, Missouri in 2011 - has killed greater than 100 people.

The severity of this epic storm has been disputed by the meteorological community for several decades. Official observations classified this tornado as F4, but damage was consistent with an F5 tornado in five of the affected towns (Rutland, Holden, Worcester, Shrewsbury and Westborough). As a result of this debate, the National Weather Service took an unprecedented step and convened a panel of weather experts during the spring of 2005 to study the latest evidence on the wind strength of the Worcester tornado. The panel considered whether to raise its designation to F5, but decided during the summer of 2005 to keep the official rating as a strong F4. The reasoning for this was that the anchoring techniques used in many of the destroyed or vanished homes could never be ascertained with certainty now, and some of these structures (many of recent postwar construction) were possibly more vulnerable to high winds than older homes. Without a proper engineering qualification, it would be nearly impossible to determine with 100% accuracy which damage was F5 and which was F4, as appearances would be similar.

Sources
  • Pletcher, Larry (2006). Massachusetts Disasters: True Stories of Tragedy and Survival. Globe Pequot. p. 240. ISBN 0-7627-3988-6.
  • Chittick, William F. (2003). The Worcester tornado: June 9, 1953. W.F. Chittick. p. 19.
  • Wallace Anthony F.C. 1956. Tornado in Worcester; an exploratory study of individual and community behavior in an extreme situation. NAS. https://archive.org/details/tornadoinworcest00wallrich Wallace's classic study on the impact of the Worcester tornado ]

Notes
  1. All losses are in 1953 USD unless otherwise noted.

References
  1. "The 25 Deadliest U.S. Tornadoes". National Weather Service Storm Prediction Center. Archived from the original on 15 May 2011. Retrieved 24 May 2011.
  2. A Look Back: The Worcester Tornado of 1953 Slide 45. National Weather Service, Taunton, Massachusetts
  3. Tornadoes of Massachusetts Past, Boston.com, July 28, 2014
  4. Pletcher 2006, p.157
  5. June 7-9, 1953 — The Flint – Worcester Outbreak
  6. "A Look Back: The Worcester Tornado of 1953". National Weather Service. Archived from the original on 27 September 2015. Retrieved 17 April 2019.
  7. "The Science Behind the Flint-Beecher Tornado: Map Features". National Weather Service. Archived from the original on 19 December 2014. Retrieved 17 Apr 2019.
  8. "1953 Beecher Tornado: Aftermath". National Weather Service. Archived from the original on 23 August 2014. Retrieved 17 Apr 2019.
  9. Heidorn, Keith, C (June 1, 2003). "The Worcester Tornado of 1953". TheWeatherDoctor. Retrieved 25 July 2010.{{cite web}}: CS1 maint: multiple names: authors list (link)
  10. Pletcher 2006, pp. 155-156
  11. Grazulis, Thomas P (July 1993). Significant Tornadoes 1680-1991. St. Johnsbury, VT: The Tornado Project of Environmental Films. ISBN 1-879362-03-1.
  12. O'Toole, John (1993). Tornado! 84 Minutes, 94 Lives. Chandler House Press. ISBN 9780963627704. Retrieved September 16, 2013.
  13. The Evening Gazette (June 10, 1953). "Tornado". The Evening Gazette. Retrieved September 16, 2013.
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