F4 St. Louis County Tornado - January 24th 1967 

DAMAGE PHOTOS

Maryland Heights  Glengate Drive

 

Chesterfield

Chesterfield Damage Photo

 Chesterfield Manor Nursing Home

Chesterfield Manor Nursing Home Damage Photo

Bridgeton Westhaven Subdivision

 St. Ann Library

St. Ann Library on St. Charles Rock Road

Ferguson  Damage Chambers Rd

Ferguson Damage - 1001 Chambers Road

 WEATHER DATA 01-24-1967

SOUNDINGS
KCOU  12Z
KCOU  00Z
KPIA  00Z
KLIT  00Z

MAP ANALYSIS
Surface 20Z
850 mb  12Z
850 mb  00Z
500 mb  12Z
500 mb  00Z

 

On January 24th 1967, a violent F4 tornado ripped a 21 mile long path of destruction across St. Louis County. It ranks as the fourth worst tornado in history to hit the St. Louis Metropolitan Area and is the last F4 tornado to affect St. Louis.

The tornado initially touched down around 6:55 p.m. in western St. Louis County at Olive Street Road near the Howard Bend Pumping Station where damage was reported to the Chesterfield Manor Nursing Home. The tornado moved northeast at 40 mph striking the small community of Lake, the luxury homes at River Bend Estates and Old Farm Estates valued between $25,000 and $33,000 (1967 dollars), Creve Coeur Meadows and Glenwood Subdivisions, and the heavily populated communities of Maryland Heights, Bridgeton, St. Ann, Edmundson, Woodson Terrace, Berkeley, Ferguson, Dellwood, the Hathaway Manor Subdivision, and Spanish Lake.  The tornado apparently dissipated or weakened as it crossed the Mississippi River, as there is no record of significant damage in Illinois.

 

The damage path ranged from 50 to 200 yards wide and the tornado was on the ground for approximately 35 minutes. Remarkably only 3 fatalities were reported while 216 people suffered injuries. Damage included 168 homes destroyed, 258 with major damage, and 1485 with minor damage. At least 600 businesses were damaged or destroyed. The total damage was estimated to be around 15 million dollars.

The tornado was given a F4 rating on the Fujita Tornado Ranking Scale. The F4 occurrence was likely small in aerial coverage with the majority of the severe damage being classified as either F2 or F3.

Eight other tornadoes struck Missouri that day with 32 tornadoes in all occurring from Oklahoma to Wisconsin.  The Wisconsin tornado is believed to be the farthest north tornado ever recorded in January. Many people will remember that the bad weather continued across Missouri January 25th and 26th with freezing rain and snow following this historic winter tornado outbreak.

NATIONAL WEATHER SERVICE (WEATHER BUREAU IN 1967)

The National Weather Service, then known as the Weather Bureau, had both its office and WSR-57 Radar located at Lambert Field. At 5:40 p.m. that evening, severe thunderstorms were detected on radar by radar operators and a severe thunderstorm warning was issued. Weather officials received a telephone call from the Creve Coeur area shortly after 7:00 p.m. and learned that a tornado was on the ground. A tornado warning was issued shortly thereafter.  

With the tornado passing just south of the airport, near the intersection of Woodson and Natural Bridge Roads, the weather office lost phone service between 7:30 and 10:00 p.m. The radar remained operational throughout the event. While the radar film for this tornado has not been analyzed in recent years, it is likely that the proximity of the tornado to the radar, the limitations of radar technology in the 1960s, and a lack of understanding about supercell thunderstorms, prevented the detection of the tornado.

TORNADO RESEARCH      ...THEN AND NOW...

Tornado research, and our understanding of tornadoes, has come a long way over the past 40 years. For instance, in an article about this tornado, the St. Louis Globe Democrat wrote,

"Tornadoes are generally caused by electric currents in the air, and are generated by high speed flow of water droplets between positive and negative clouds".

Today, we know that most violent tornadoes occur with supercells, which are rotating thunderstorms with a well-defined radar circulation called a mesocyclone. While the exact mechanism that produces tornadoes still remains unknown, it is believed that tornado formation is dictated mainly by things which happen on the storm scale, in and around the mesocyclone.

Recent theories, and research from the VORTEX program, suggest that once a mesocyclone has developed, tornado development is related to the temperature differences around the edge of the downdraft air wrapping around the mesocyclone.  However, other studies suggest that tornado formation can happen without such temperature patterns.

Meteorologists Mark Britt and Fred Glass at the National Weather Service in St. Louis continue to research and document tornado climatology for the St. Louis county warning area. Over the last year, they have focused their attention on the strong (F2-F3) and violent (F4-F5) tornadoes that have occurred within the cool season. Climatology shows that when tornadoes occur during the months of November, December, January, and February, nearly half of them are either strong or violent. Therefore, there is a greater likelihood for tornadoes that occur during the cool season to be strong or violent when compared to the rest of year.  They presented a poster at the 2006 Severe Local Storms Conference titled, "Environmental and Synoptic Conditions Associated with Cool Season Strong and Violent Tornadoes in the North Central United States".


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