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THE BLIZZARD THAT CHANGED THE NWS...

November 11th, 1940, one of the worst winter storms ever seen whiplashed the upper Midwest. Occurring on Armistice Day, the freak storm killed 154 and became legendary as "the Armistice Day Blizzard". It's fury and lack of warning caused a public uproar that changed the face and operation of the what was then known as the U.S. Weather Bureau.

While I'm too young to remember the storm, it wouldn't matter anyway as its impacts where I grew up in eastern Iowa were confined to wind, a dramatic drop in temperatures, and a few flurries. Not far away though, the blizzard threatened life, livestock, and wildlife, bringing the world to a standstill for up to a week in parts of rural Minnesota. Today is the 83 year anniversary of this incredible event, a storm that I believe for November 11th is unmatched in intensity and impact. It arguably is the G.O.A.T. (the greatest blizzard of all-time) to strike the Midwest.

Barricades of snow in Madison, Minnesota November 1940


Jeff Boyne of the NWS in La Crosse, Wisconsin put together a fantastic summary of the factors and conditions that drove the event and how it ultimately changed the function of what today is called the National Weather Service. Some excerpts of Boyne's are included below. To get Jeff's full report you can follow this link. https://www.weather.gov/arx/nov111940 Otherwise, to find out more about the explosive power of the storm, read on.


THE COLD HARD FACTS

On November 11, 1940, a rapidly deepening low pressure system moved northeast from Kansas City, MO northeast through the Upper Mississippi River Valley and into the Upper Great Lakes. This low pressure area produced the lowest pressure reading ever recorded up to this time at Charles City, IA (28.92 inches), La Crosse, WI (28.72 inches), and Duluth, MN (28.66 inches). Armistice Day (now known as Veteran's Day) began for many with patches of sunshine and temperatures in the 40s and 50s. The weather forecast for that morning was for colder temperatures and a few flurries. The day was so nice that duck hunters dressed in short-sleeved shirts rushed to the marshes along the Mississippi River early that morning.


During the late morning and early afternoon, a strong cold front moved through the region. Behind this front, the weather became rather blustery and the temperature plunged to the single digits by the next morning. Rain turned to sleet and eventually to driving snow. Twelve duck hunters were trapped on the Mississippi River between St. Paul and Prairie du Chien by gale-force winds and threatening waves. These hunters sought shelter on small islands and eventually froze to death. Rescue work the next day was hindered by ice which had developed during the preceding night.

Minneapolis Star Tribune November 1940

Minneapolis Star Tribune November 1940


Elsewhere heavy snow fell across the Dakotas, much of Minnesota and western Iowa, and northwest Wisconsin. The greatest snow total was 26.6 inches in Collegeville, MN. In addition, 30 to 50 mph+ winds caused considerable blowing and drifting of snow which trapped unsuspecting motorists.

Watkins, Minnesota November 11, 1940 John McNab

Twenty foot drifts were reported near Willmar, MN. The blizzard left 49 dead in Minnesota, and gales on Lake Michigan caused ship wrecks resulting in another 59 deaths. In total, the storm claimed a total of 154 lives, and killed thousands of cattle in Iowa. More than a million turkeys were killed by the storm in Wisconsin, Minnesota, and other states. The blizzard became know as the “Armistice Day Storm”.

Watkins, Minnesota following the Armistice Day Blizzard 11/11/1940


This storm, along with a slow moving blizzard which would move across northern Minnesota in mid March 1941, caused the Weather Bureau to rethink its forecasting procedures. Forecasting for the entire region had been directed by the Chicago office, but in the wake of this storm, responsibilities were distributed to regional centers to provide more timely and accurate predictions. More on the aftermath and repercussions later.


THE METEOROLOGICAL SET-UP

Preceding Armistice Day, a strong weather system moving into the Pacific Northwest had taken down the Tacoma Narrows Bridge. Until the collapse on November 7, 1940 the bridge had been the 3rd longest suspension span in the world. The Tacoma Narrows Bridge, an engineering wonder, had already acquired the name Galloping Gertie due to its motion in the wind. A four mile an hour breeze could start oscillations in the bridge while stronger breezes often had no effect. On November 7, 1940 winds of 35 to 45 mph caused the center span to undulate 3-5 feet and the bridge failed before the center of the storm system reached shore. On November 8, 1940 the storm center remained off the Washington coast producing gale force winds. Meanwhile pressure was falling over the Pacific Northwest.

The path of the Armistice Day storm


By November 10th the storm system had moved across the Rocky Mountains to redevelop over Trinidad Colorado (Knarr, 1941). Initially the system pushed east then it curved northward into the central United States where it would leave a path of icy destruction. During the next 6 hours the storm center moved to the vicinity of Iowa Falls, Iowa. West of the center blizzards raged across South Dakota and a widespread ice storm across Nebraska left hundreds of people impacted by the storm. East of the center a broad swath of warm air streamed up the Mississippi Valley.

Weather map 6:30am November 11, 1940


During the day and into the night severe weather erupted across much of the Midwest. A tornado was reported one mile west of Davenport Iowa, 2-3 inches of heavy rain fell in spots over the Mississippi Valley, and heavy snow began to fall across Minnesota and Western Iowa. Gale velocities were measured at 80 mph at Grand Rapids, Michigan, and were estimated to be even higher over the lakes. By the time the storm was centered over Lake Superior, the barometer reading had plummeted to 28.57 inches of mercury.

Weather Map 12:30pm November 11, 1940


SNOW REPORTS


On November 10, 1940, a weak low pressure system (ahead of the Armistice Day low pressure system) began to produce light snow across northern and western Minnesota, and northern Wisconsin. The snow rates then rapidly increased on the morning of November 11th as a much stronger low pressure system moved from Kansas City, MO to just north of La Crosse, WI. The heavy snow then continued to fall into the afternoon into the morning of November 12th as the low pressure system continued to strengthen and move slowly northeast into northern Ontario. In addition to the snow, sustained 30 to 50 mph winds caused considerable blowing and drifting of snow which trapped unsuspecting motorists. Below you can see where snow accumulated.

In Iowa, the snow was mainly confined to the western and northern parts of the state. The highest snow total was 13 inches in Cushing.

In Minnesota, the heaviest snow fell from southwest and south central parts of the state northeast into the Arrowhead. The highest snow total was 26.6 inches Collegeville.

In Wisconsin, the heaviest snow fell across the northwestern parts of the state. The highest snow total was 19 inches six miles north of Bayfield.


Excelsior Boulevard, west of Minneapolis after the Armistice Day Storm: Minnesota Historical Society


RECORD LOW BAROMETRIC PRESSURE

EXTREME WINDS


Stalled Passenger Train near Granite Falls, Minnesota. November 1940-Minneapolis Star Tribune


CONSEQUENCES OF THE EVENT


Prior to the Armistice Day Storm of 1940:

Weather observations, forecasts and warnings were much different in 1940 and so were the ways people received information. Until 1934 the Weather Bureau offices operated 12-15 hours a day with two basic observations taken at 8 a.m. and 8 p.m. The observations were transmitted via telegraph. There were no satellite images and few upper air observations. In the Midwest the Chicago District issued weather forecasts for Illinois, Indiana, Iowa, Michigan, Wisconsin, Minnesota, North Dakota, and South Dakota. Weather Bureau forecasts, which were issued mid morning and mid evening, were brief and general. Distribution methods ranged from reports in newspapers, on cards displayed in the lobbies of public buildings, radio broadcasts, or by telegraph. Cold wave warnings which were prepared for citrus fruit growers, cranberry, tobacco interests, and iron ore shippers were based upon forecasters recognizing a particular weather pattern and its potential effect. Weather Bureau offices in cities like Davenport and Dubuque provided weather observations which were sent to the district offices via teletype. A wealth of weather observational records which had been accumulated since the 1800’s were basically underutilized until computers improved the ability to record and retrieve data. During the modernization of 1934 card punching of weather data began and phone calls to Weather Bureau offices increased to about 100 phone requests a day for climate information (Whitnah, 1961). In 1938 a “breakfast forecast” was introduced, and predictions were revised four times a day (4 a.m. & 4 p.m., 10 a.m. & 10 p.m.). For rural communities weather information was limited, but certainly available, since it was common for telephone operators and carriers on rural free delivery mail routes to distribute this information (Whitnah, 1961). In 1940 long range forecasting was introduced. This longer forecast, which covered 5 days and which was issued twice a week, was based upon upper air pressure data and correlated with past weather patterns (Whitnah, 1961).


After the Armistice Day Storm of 1940:

In the days and weeks after the storm, the U.S. Weather Bureau responded to criticism that it failed to predict the huge blizzard. Officials said they knew a storm was coming, but were wrong about its strength and scope. Perhaps the most embarrassing revelation was that no one was watching the storm's explosive development in the pre-dawn hours of November 11 (the low pressure deepened 1-2 millibars per hour over a 24 hour time period). A retired government forecaster says the Midwest headquarters in Chicago was not staffed overnight. The uproar led to several changes:

  1. It strengthened support to keep weather offices open 24 hours a day (the Chicago office went to round-the-clock operation).

  2. Prior to the storm, forecasting for the entire region had been directed by the Chicago office, but in the wake of this storm, responsibilities were distributed to regional centers (Twin Cities branch was upgraded so it could issue forecasts) to provide more timely and accurate predictions.

"The Armistice Day Storm remains noteworthy to society because it was a seminal event that continues to impact humans. Anything that endures as part of a culture from one generation to another is considered a seminal event; and the societal impacts of such an event can change lives and change history. The consequences of societal impact alter the ways in which people live, work, play, relate to one another, organize to meet their needs and generally cope as members of society. Forecasters must assess the potential for societal impacts when they strive to understand the atmospheric environment, timing of an event, and the social environment in their warning areas. Any event with the potential for folk-lore will produce societal impact. The longer we accumulate weather records the more likely we are to find extreme weather events. An assessment of societal impacts has the potential to help individuals and communities understand and anticipate possible social consequences of an event in regards to human populations. It is becoming standard practice to weave social science into weather and climate research (Gruntfest & Lazrus, 2009). Over time public perceptions are changed partly due to massive growth in media coverage, but also because real-time media with gripping images bring storm and disasters into our living rooms. Generations have based their understanding of extreme winter weather against the storm that struck on Armistice Day 1940. Seventy years later the Armistice Day Blizzard remains the second most requested bit of information from the Minnesota State Climatologist office (Boulay, 2009). In Iowa this catastrophic event changed agricultural growing practices as apple growers switched from tending orchards to corn and soybean production. Evidence of the Armistice Day Blizzard is recorded in newspaper clippings, photos, museum collections, and stories of this event have been captured in cookbooks, journal articles, and passed on through family oral traditions. This storm produced an impact on society due to the death and destruction left in its wake. If one measures the impact of an event by the diversity of the information that remains this storm was indeed memorable."


Again, my thanks to Jeff Boyne of the NWS in La Crosse, Wisconsin for allowing me the luxury of incorporating his hard work and research into this post. Often times I have wondered what it would be like to experience a blizzard of such magnitude, especially November 11th. So far that day has never come for me (or for that matter anybody else). 83 years later the blizzard is still unrivaled and the benchmark winter storm that all others are measured by. One thing I can safely say, is thanks to this event and the advancement of meteorology, the storm today would be predicted days in advance and the loss of life would have been significantly less. That is a very good thing. Roll weather...TS


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