1913 Omaha Easter Sunday tornado
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The tornado outbreak sequence of March 1913 was a devastating
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of
tornado outbreak __NOTOC__ A tornado outbreak is the occurrence of multiple tornadoes spawned by the same synoptic scale weather system. The number of tornadoes required to qualify as an outbreak typically are at least six to ten, with at least two rotational l ...
s that affected the northern Great Plains, the
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, and sections of the upper Midwest over a two-day-long period between March 21–23, 1913. Composed of two outbreaks, the sequence first began with a tornado outbreak that commenced in
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early on March 21. Several significant tornadoes occurred, one of which killed seven people in one family and another destroyed much of Lower Peach Tree,
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, with 27 deaths all in that town. The tornado at Lower Peach Tree is estimated to have been equivalent to a violent F4 tornado on the
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, based upon damage accounts. The tornadoes occurred between 0630–1030 UTC, or pre-dawn local time, perhaps accounting for the high number of fatalities—a common trend in tornadoes in the
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.Robinson, "Natural Disasters", ''Encyclopedia'', p. 584 In all, tornadoes in Mississippi,
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, and Alabama killed 48 people, perhaps more, that day and injured at least 150 people. March 23,
Easter Sunday Easter,Traditional names for the feast in English are "Easter Day", as in the ''Book of Common Prayer''; "Easter Sunday", used by James Ussher''The Whole Works of the Most Rev. James Ussher, Volume 4'') and Samuel Pepys''The Diary of Samuel P ...
, was the most violent tornado outbreak to affect the northern Great Plains on so early a date in the year—a record that still stands as of 2020. That day, four F4 tornadoes affected portions of eastern Nebraska and western Iowa, killing at least 168 people. The deadliest tornado of the day was a potent F4 tornado that grew to in width as it passed through northern Omaha,
Nebraska Nebraska () is a state in the Midwestern region of the United States. It is bordered by South Dakota to the north; Iowa to the east and Missouri to the southeast, both across the Missouri River; Kansas to the south; Colorado to the sout ...
, killing at least 94 people in the city proper and three in rural areas. Damage in Omaha reached at least F4, possibly even F5, intensity, though confirmation of F5 damage could not be determined from available evidence. The tornado is the 13th deadliest ever to affect the United States and the deadliest to hit the U.S. state of Nebraska as of 2014. No other violent tornado would affect Omaha for another 62 years. Outside the Great Plains, the outbreak of March 23 also produced two other F4 tornadoes, one each in
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and
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, including a devastating path more than through southern Terre Haute, Indiana, killing 21 people and injuring 250. In all, the two consecutive outbreaks killed at least 241 people and caused at least 19 tornadoes, though only significant events were recorded and other, weaker tornadoes may have gone undetected. The outbreak sequence also produced seven violent tornadoes, nearly half the documented total of tornadoes for the sequence. Tornadoes struck Nebraska, Iowa,
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, Missouri,
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, and Indiana. At least $9.68 million in damages were reported.


Background

A series of potent storm systems traversed the US during March 1913, described by the US Weather Bureau as "...the most extraordinary situation in regards to the weather since the creation of the bureau." Anomalously high moisture had gathered near the US Gulf Coast, as an intense upper level storm system moved in from the west. According to retrospective numerical modeling of this event, a strong cap aloft was in place over the central Plains, as is common as the elevated mixed layer advects eastward from the Rockies. Observations taken at 13Z 23 March 1913 showed that surface low pressure was located in Colorado, and a
warm front A warm front is a density discontinuity located at the leading edge of a homogeneous warm air mass, and is typically located on the equator-facing edge of an isotherm gradient. Warm fronts lie within broader troughs of low pressure than cold f ...
stretched due eastward from there into Illinois. Morning temperatures near this front were in the 30s. South of the front warmer and moister air was present, but dewpoints in the upper 50s were confined to southern Oklahoma and Arkansas, far away from where the tornadoes were to later occur in eastern Nebraska and western Iowa. As the day progressed, the surface low ejected through Nebraska, with a
dry line A dry line (also called a dew point line, or Marfa front, after Marfa, Texas) is a line across a continent that separates moist air and dry air. One of the most prominent examples of such a separation occurs in central North America, especially ...
and trailing
cold front A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface trough of low pressure. It often forms behind an extratropical cyclone (to the west in the Northern ...
. South winds blowing 40-50 knots at times brought the moister air rapidly northward. One of the worst dust storms on record occurred behind the dry line in western Kansas, but in the warm sector the day remained dry until mid afternoon when light showers began to form in central Nebraska. A cooperative observer in Osceola noted that the wind shifted from S to NW at 2230Z (4:30 PM local). Professors at the University of Nebraska at Lincoln noted that the relative humidity there jumped from 53% at 2150Z to 78% at 2230Z, indicating much higher dewpoints had rapidly arrived in Lincoln since the cold front was still to the west near Osceola. They also noted that the surface low passed just to the north of Omaha and was in western Iowa at 01Z 24 March 1913. With all of this observed information, it is likely that the quality moisture required to produce convection strong enough for tornadoes arrived just an hour or two before the strong forcing associated with the surface low pressure and attendant frontal systems. At the time of the tornadoes it is estimated that surface temperatures were in the upper 60s, dewpoints were in the upper 50s, and surface winds were southerly around 25-30 knots. Numerical modeling estimates that 500 hPa flow was around 80 knots from the WSW and that CAPE was from 1000–2000 J/kg. These conditions are similar to those found in other tornado outbreaks. Tornadic storms developed from 5:00-6:00 PM local time and while storm motions were to the NE, the prevalence of tornadic storms moved southward with the
dryline A dry line (also called a dew point line, or Marfa front, after Marfa, Texas) is a line across a continent that separates moist air and dry air. One of the most prominent examples of such a separation occurs in central North America, especially ...
/
cold front A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface trough of low pressure. It often forms behind an extratropical cyclone (to the west in the Northern ...
intersection, lasting until 8:00 PM local in NW Missouri. A serial
derecho A ''derecho'' (, from es, derecho, link=no , 'straight') is a widespread, long-lived, straight-line wind storm that is associated with a fast-moving group of severe thunderstorms known as a mesoscale convective system. Derechos can cause hurri ...
then formed and moved across Iowa and Illinois through the nighttime hours, hitting Chicago in the early morning.


Outbreak statistics


Confirmed tornadoes


March 21 event


March 23 event


Omaha, Nebraska

The Omaha
Easter Sunday Easter,Traditional names for the feast in English are "Easter Day", as in the ''Book of Common Prayer''; "Easter Sunday", used by James Ussher''The Whole Works of the Most Rev. James Ussher, Volume 4'') and Samuel Pepys''The Diary of Samuel P ...
tornado struck
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, at approximately 6:00 p.m. on March 23, 1913. The storm's path was reported as being wide and contained multiple vortices. The Omaha tornado followed the path of
Little Papillion Creek Papillion Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed March 30, 2011 tributary of the Missouri River in Nebraska. Its watershed lies in Washington, Douglas and Sarpy coun ...
as it entered the city. It moved through the west side of town alongside the
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, destroying the small workers cottages in the area. The tornado was so strong that steel train cars were later found pierced by pieces of shattered lumber from the demolished homes. By the time the tornado reached Dewey Avenue it was five blocks wide. When it reached Farnam Hill, the tornado followed a shallow valley through this upscale neighborhood. The large mansions of Farnam were no match for the winds, and many houses were torn to pieces, along with several in the Gold Coast Historic District including the
Joslyn Castle The George and Sarah Joslyn Home (officially named "Lynhurst," and known locally as Joslyn Castle), is a mansion located at 3902 Davenport Street in the Gold Coast Historic District of Omaha, Nebraska, United States. Built in the Scottish Baron ...
, which sustained considerable damage. Buildings were found chopped in half, pipes and supports dangling into space, such as the Duchesne Academy which was nearly obliterated. At North 24th and Lake Streets in the Near North Side neighborhood a large
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crowd was enjoying an Easter Sunday performance when the tornado flattened the building and killed more than two dozen people. Other brick structures in this small commercial district took similar hits, and more people died here than in any other part of Omaha. A streetcar running down North 24th Street in
North Omaha North Omaha is a community area in Omaha, Nebraska, in the United States. It is bordered by Cuming and Dodge Streets on the south, Interstate 680 on the north, North 72nd Street on the west and the Missouri River and Carter Lake, Iowa on the ...
encountered the tornado near this area. Thanks to the quick action of operator Ord Hensley in ordering passengers to lie on the floor of the car, everyone survived. Later, photographers would spot the wrecked machine and would call it the "Streetcar of Death", imagining that no one on board could have survived given the immense damage. The F4 tornado skirted the downtown area and moved over the Missouri River into Iowa, causing further damage before dissipating. In all, 103 people died, 94 of which were in Omaha, and another 400 were injured. Reportedly, 2,000 homes in Omaha alone were destroyed, with $8 million total damage from the storm, $5.5 million of which was in Omaha (financial damage estimates vary; the NOAA reports more damage than this). In the aftermath of the tornado, a
cold front A cold front is the leading edge of a cooler mass of air at ground level that replaces a warmer mass of air and lies within a pronounced surface trough of low pressure. It often forms behind an extratropical cyclone (to the west in the Northern ...
moved into Omaha and caused further misery, as newly homeless residents struggled to escape the snowy weather. Many homes throughout the northern side of the city were leveled, and some were swept away. Photographs at the time showed empty foundations, which possibly indicated F5 damage, but these may have been related to post-tornado clean-up.


Non-tornadic effects

The same storm system that struck Nebraska created a dust storm in
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and hit
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with hail and heavy rain. The Omaha tornado marked the beginning of the destruction from storms associated with the
Great Flood of 1913 The Great Flood of 1913 occurred between March 23 and March 26, after major rivers in the central and eastern United States flooded from runoff and several days of heavy rain. Related deaths and damage in the United States were widespread and ext ...
. On Monday and Tuesday, March 24 and 25, the storms brought heavy rains to the Midwest and upstate New York, causing widespread flooding.


Aftermath

Remarkably, operators from the
Webster Telephone Exchange Building The Webster Telephone Exchange Building is located in North Omaha, Nebraska. It was designed by the well-known Omaha architect Thomas Rogers Kimball. After the Easter Sunday Tornado of 1913, the building was used as the center of recovery operatio ...
in Omaha did not leave their stations either during or after the tornado. The building was used as an infirmary for the wounded and dying, with physicians and nurses coming from area hospitals.
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troops from
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set up headquarters in the building, as soldiers patrolled the area for looters and to offer assistance. Initially, James Dahlman, the longtime mayor of Omaha, refused assistance from any outside sources, including the federal government. However, he relented after seeing the extent of the damage throughout the city. The federal government poured in assistance soon after. The massive damage caused by the tornado inspired new engineering techniques aimed at creating a tornado-proof edifice. The first such building was the First National Bank of Omaha building, built in 1916 at 1603 Farnam Street. The 14-story building was built in a "U"-shape.


See also

* 2020 Easter tornado outbreak - Another deadly tornado outbreak during Easter weekend 107 years later. * Disaster Books – Omaha Easter Sunday Tornado *
Great Dayton Flood The Great Dayton Flood of 1913 resulted from flooding by the Great Miami River reaching Dayton, Ohio, and the surrounding area, causing the greatest natural disaster in Ohio history. In response, the General Assembly passed the Vonderheide Act to ...
*
List of North American tornadoes and tornado outbreaks These are some notable tornadoes, tornado outbreaks, and tornado outbreak sequences that have occurred in North America. #''The listing is U.S.-centric, with greater and more consistent information available for U.S. tornadoes. Some North Americ ...
*
List of tornadoes causing 100 or more deaths This is a list of the deadliest tornadoes in world history. This list includes confirmed individual tornadoes that caused 100 or more direct fatalities. The deadliest tornadoes by far have occurred in a small area of Bangladesh and East India. In ...
*
List of tornadoes striking downtown areas This article is a list of tornadoes that have impacted the central business district (downtown or city center) of a large city (that is, one having at least 50,000 people, not counting suburbs or outlying communities, at the time of the storm). I ...
*
Timeline of North Omaha, Nebraska history Significant events in the history of North Omaha, Nebraska include the Pawnee, Otoe and Sioux nations; the African American community; Irish, Czech, and other European immigrants, and; several other populations. Several important settlements an ...


Notes


References


Bibliography

* * *''Encyclopedia of Southern Culture'', Vol. I, ed. Charles Reagan Wilson and William Ferris (New York: Anchor Books, 1989). *


External links


National Oceanic and Atmospheric Administration
*(n.d.

''Tragic Story of America's Greatest Disaster''. {{DEFAULTSORT:1913-03-21 tornado outbreak F4 tornadoes by date ,1913-03-21 Tornadoes of 1913 Tornadoes in Nebraska Natural disasters in Omaha, Nebraska North Omaha, Nebraska Omaha Easter Sunday tornado 1913 natural disasters in the United States March 1913 events in the United States