From May 10âÂÂ12, 2014, a large and widespread tornado outbreak of 44 tornadoes spanned across portions of the central and Great Plains regions of the United States. The May 11 portion is sometimes referred to as the Mother's Day tornado outbreak by locals, due to it occurring on the celebration at the time. The outbreak began on the 10th, with isolated tornadoes across Idaho, Kansas, Missouri and also Alabama. The strongest tornado of that event was an EF2 tornado that struck Orrick, Missouri, causing widespread damage in town.
The following day on the 11th, dozens of tornadoes were reported across Kansas, Nebraska, Iowa and South Dakota, with the event's epicenter taking place across southern and eastern Nebraska, where a prolific and cyclical, high-precipitation supercell produced 17 tornadoes from areas southeast of Hastings, to the Omaha metropolitan area. Two large EF3 tornadoes caused severe damage to portions of Clay, Fillmore, York and Seward counties. The first one impacted rural farmsteads until eventually passing by Sutton. The parent supercell brought in powerful rear flank downdraft winds that were estimated at into the downtown area. The second EF3 was a massive and rainwrapped wedge tornado, which spanned wide and struck farms near Cordova, before eventually making a direct hit on the small city of Beaver Crossing. Severe rear flank downdraft and inflow winds occurred alongside as well as the supercell tracked through southeastern Nebraska. Winds of were reported near the Omaha metro area, notably Douglas County.
On the 12th, minor tornadic activity was reported. Only two tornadoes, both rated EF0 occurred outside of Elyria and Medina, Ohio, before the outbreak came to an end.
Alongside tornadic events, major and historic flash floods caused by an organized convective complex struck northern Ohio on May 12. A winter storm brought heavy snow cover for parts of the Rocky Mountains and High Plains. of snow was reported at the Sierra Madre Range, Wyoming. One person was killed along US 285 near Denver, Colorado by the storm.
Only one person was injured by one of the tornadoes from this outbreak. Other injuries were inflicted by the winter storm that persisted through May 10âÂÂ12, where one death also occurred.
On May 9, 2014, at 11:30 p.m. CDT (04:30 UTC), the Storm Prediction Center outlined a slight risk for severe weather across portions of Missouri, Illinois, Indiana, Kentucky, Tennessee, and Arkansas. A 2% probability for tornadoes within of a point within the region was also outlined, as a cold front moved eastward through the Great Lakes region and the Ozarks into an environment with moderate atmospheric instability and strong wind shear.
By May 10, 1:00 a.m. CDT (06:00 UTC), the slight risk shifted westward, including much of the central Great Plains region, with a 5% probability for a tornado within of a point within portions of northwest Missouri and northeast Kansas, where increasing temperatures and maximized low-level shear along a warm front enhanced the threat for tornadoes. As the day progressed further, several supercell thunderstorms formed along a front over areas in central Missouri, producing several tornadoes and bringing strong wind and hail to the region. Additionally, an isolated tornado was reported in the northeastern parts of Idaho.
On May 11, 1:00 a.m. CDT (06:00 UTC), a moderate risk was outlined for portions of northeast Kansas, southeast Nebraska, northwest Missouri, and much of southwest and central Iowa, in light of the ample moisture and high temperatures ahead of a warm front within the region. A 10% probability for a tornado within of a point was highlighted for much of the same area. Alongside this, a slight risk was outlined, stretching from central Texas to the Great Lakes region, alongside a 2% and 5% hatched area for tornadoes overlapping much of same areas. At 3:00 a.m. CDT (08:00 UTC), a line of strong thunderstorms rapidly formed near the Kansas/Nebraska border and shifted northward, bringing strong wind and hail to the area. As the day progressed, the moderate risk area was expanded to include more of the central Great Plains region, with a 15% hatched area for tornadoes being outlined for portions of southwest Iowa and southeast Nebraska, as strong, low-level wind shear, considerable moisture, and moderate instability favored supercellular development across the region. In the afternoon hours, thunderstorms began to rapidly develop near Hastings, Nebraska, with one severe storm that was moving eastward along a warm front producing numerous tornadoes across the region, including two that were rated EF3. Strong wind gusts, heavy rain, and large hail were also reported. Additional supercells moved across the Central Plains region, stretching from central Kansas to central Iowa. Very large hail was reported, alongside numerous tornadoes and damaging winds.
On May 12, 1:00 a.m. CDT (06:00 UTC), a slight risk was outlined for a large portion of the southwestern and midwestern regions of the United States, stretching from southern Texas to the Great Lakes region, as moderate atmospheric instability redevelops and a cold front that was over portions of Iowa, eastern Kansas, and central Oklahoma. A 2% probability for a tornado within 25 mi (40 km) of a point was outlined for much of the same areas, alongside a 5% hatched risk area for central-to-northeast Missouri, eastern Iowa, northwestern Illinois, and southwest Wisconsin. Clusters of strong thunderstorms began to develop that afternoon, affecting areas from southern Michigan to the southern Great Plains. Strong wind and hail were reported across the region, alongside several tornado reports. That evening, a warm front over Lake Erie tracked over Ohio, with several embedded supercells forming over north-central portions of the state. The slow-moving storms produced two confirmed tornadoes and extreme levels of rainfall, resulting in numerous flash floods.
A supercell formed over the Kansas City metropolitan area, dropping this strong tornado on the northern bank of the Missouri River, near Sibley in Jackson County. It first began causing EF0 damage to trees in this area, before moving out of Jackson County, where it would intensify to EF1 strength, snapping or damaging powerlines along Egypt Road. As the tornado was west of Orrick, the National Weather Service forecasting office for the Kansas City, Missouri area issued a tornado warning for parts of Ray County at 5:30 p.m. CDT (12:30 UTC).
The tornado would begin to close in on Orrick, parallel to MO 210. Upon entering the small city, the tornado would cause EF1 damage to a stick-built pole barn on Sibley Road. One home had its garage and side walls blown out, windows shattered and roof damaged. Entering the main part of Orrick, the tornado began to intensify and cause EF2 damage to a house, which had its roof ripped off. At the same time, the tornado nearly destroyed much of the city's high school, with the roof for a majority blown off. EF1 damage was inflicted for nearly the entirety of Orrick as the tornado traversed through. Upon exiting, the tornado weakened and remained at EF0 intensity. Rear flank downdraft winds estimated at snapped trees along State Highway T within Fleming. After passing north and east of Camden, the tornado would dissipate to the southwest of Henrietta. The supercell responsible for this tornado produced an EF0 tornado north of Lexington, and an EF1 tornado northeast of Marshall.
The event was the first notable tornado of the outbreak, directly striking the city of Orrick. 80% of the structures in Orrick suffered damage by the tornado, blocking off access to the city. This tornado tracked for , and had a width of across Jackson and Ray counties. In light of the damage, Orrick High School was closed for the remaining school year, and the school's senior class had their graduation ceremony in Excelsior Springs.
The first major tornado on Mother's Day touched down north-northwest of Fairfield, in central Clay County. This large, multiple-vortex tornado descended from a low-based supercell, which brought darkness early on into the afternoon hours as it passed south of Clay Center at EF0 intensity. The tornado then began to strengthen to EF1 intensity east of the town, accompanying rear flank downdraft winds swept across portions of Clay County, damaging or destroying several trees and powerlines. Farming equipment, especially irrigation pivots were flipped and or severely totaled by both the tornado and accompanying rear flank downdraft.
After tracking for , the tornado enlargened in width, and briefly intensified further to the south of Saronville, causing EF2 damage to several trees, which had their trunks snapped. EF1 damage persisted as many barns were heavily destroyed, and rural homes suffered minor damage. West of Sutton, the tornado caused considerable EF2 damage to a pole barn. The tornado would then begin to curve around the small city from the west, with predominantly EF1 damage inflicted on homesteads. North of Sutton, along Road X, the tornado became intense as it impacted farmstead at EF3 intensity. A poorly-built residence was completely leveled, with debris filling up the basement. EF2 damage was inflicted to several utility poles, and one outbuilding that had limited anchoring the was partially swept off its foundation. For the remainder of its time, the tornado caused EF1 damage to multiple homes along the Clay-Fillmore County border, before it weakened and dissipated north of US 6 in Fillmore County.
This was the first significant tornado produced by the prolific supercell that tracked across southeastern Nebraska. Many homes and farms were impacted by this large and often obscured tornado, which tracked for across the two counties, and was at its widest. A total of $14 million (2014 USD) was caused by this tornado, making it the most costly event of the entire outbreak. Rear flank downdraft winds of around impacted the downtown area of Sutton, causing major and widespread damage throughout the city.
This severe tornado began just south on the Fillmore-York County border, north of Exeter. The tornado began at EF1 intensity, as it flipped an irrigation pivot onto fleeing storm chasers. After entering York County, the tornado widened and intensified to EF2 strength as it began to snap utility poles and destroy barns west of Cordova. At the same time, the parent supercell's rear flank downdraft produced estimated winds at , which damaged powerlines and outbuildings across eastern Fillmore and York counties.
As the tornado crossed over into Seward County, it began to pass north of Cordova and intensify to EF3 strength, impacting two homesteads on County Road 462. One farmhouse only had its inner walls standing, and a nearby barn was completely destroyed at one of these properties as well. The tornado continued causing EF3 damage as another farmhouse on Denton Road suffered major damage to its exterior walls, with only the interior room standing. Two satellite tornadoes also formed one after another north of the EF3 tornado.
The ongoing rear flank downdraft, with near mid-range EF2-equivalent winds continued to impact many rural areas to the south of Beaver Crossing, with the tornado also becoming heavily rainwrapped and approaching the village. Making a direct hit, the tornado engulfed the entirety of Beaver Crossing, causing widespread EF2 damage to numerous homes and businesses with most having lost their roofs or covering at the worst. After leaving Beaver Crossing, the tornado continued causing EF2 damage to rural structures, notably one home southeast of town was considerably destroyed. After tracking for a few miles, the tornado ended south of Goehner. A large EF2 tornado already formed 5 minutes prior, and became the dominant circulation as the EF3 tornado was dissipating.
This massive and rainwrapped wedge tornado, which spanned wide was the sixth, and largest tornado the prolific supercell that traveled across southeastern Nebraska produced, and of the entire outbreak. It tracked for across Fillmore, York and Seward counties for over half an hour. Monetary losses totaled up to $11.4 million (2014 USD), making it the second most damaging tornado of the outbreak. Volunteers came in to help residents of Beaver Crossing, with former Nebraska governor Dave Heineman visiting the area the next day on May 12.
During the May 11 event, a long-lived supercell that produced over a dozen tornadoes across southeastern Nebraska, produced a large swath of powerful rear flank downdraft (RFD) winds across portions of Clay, Fillmore, York, Seward, Lancaster and Saunders counties. These severe winds sometimes exceeded , with the highest gusts at during the ongoing tornadoes. RFD winds of completely damaged the downtown area of Sutton, with multiple homes, businesses and outbuildings suffering from major roof loss, to total collapse of the structures themselves. Winds of were reported near the Omaha metro area as this supercell neared by.
On May 12, destructive flash floods took places in the northern parts of Ohio, particularly Lorain County, which was among the hardest hit area. The floods were caused by an organized convective complex, with embedded supercells that formed over Lake Erie from a warm front. These storms were very slow-moving, which caused them to pour inches of rainfall across numerous communities. County-level emergencies were declared for Lorain, Medina and Summit counties. In Cuyahoga County, rescue operations were conducted, however, no casualties were reported. Lorain County saw up to of rainfall occur in 3.5 hours, with an estimated 300 homes and 1000 businesses destroyed. In Summit County, fell over Cuyahoga Falls. Around of floodwater was reported in basements of homes, by the Medina County Emergency Management Agency. The intensity of the rainfall was a historic, half-millennium event for some of the most damaged areas.
From May 10 to 14, a rare late-season winter storm occurred over the central Rocky Mountains and High Plains. Areas in western Nebraska, Wyoming, Colorado and Utah were impacted by the snow storm. Over of snowfall across multiple locations. The highest measured was at Divide Peak, at the Sierra Madre mountain range in southern Wyoming, which saw of snow. Other places with heavy measurements were near Pinecliffe, Colorado, a measurement of of snow occurred. In Leadville, Colorado and Arlington, Wyoming; of snow was recorded. Heavy wet snow damaged trees in Cedar City, Utah. According to Xcel Energy, up to 17.000 customers lost power during the morning hours of May 12. Denver International Airport was among the many that suffered from the power outages, but the impact was kept at minimum due to a backup generator. Travel and transportation across the Rockies were severely hampered and became dangerous throughout the duration of the storm. Flights at airports in the impacted regions saw delays or cancellations. One death occurred by winter storm on US 285, near Denver, Colorado. In Wyoming, I-80 was issued to be closed off. This prompt caused thousands of motorists to be stranded, and rest stops along the interstate were overcrowded.