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2014 Pilger tornado family

Series of EF4 tornadoes in Northeast Nebraska

  • 16 min read
  • 4 chapters

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Through Confluence

The first tornado touched down in an open field near Stanton but quickly dissipated. A more significant tornado then formed near Stanton. This tornado traveled for approximately 12 miles, causing extensive damage to several farmsteads and sweeping away a few farmhouses before lifting north of Dewey. Shortly thereafter, the supercell produced two additional violent tornadoes, subsequently becoming twin EF4 tornadoes. One of these tornadoes struck the village of Pilger directly, resulting in devastating damage and one death. The other twin over to the east leveled a farmhouse before dissipating east of Altona, Nebraska, responsible for a second fatality. Meanwhile, the western twin tornado, which devastated Pilger earlier, continued to wreak havoc across farmlands before eventually being absorbed by the Wakefield tornado. The final violent tornado from the supercell swept away three farmhouses and inflicted significant damage on multiple other farmsteads before dissipating north of Wakefield. The sixth and last tornado produced by the supercell was weak and short-lived.

Meteorological setup

Episode narrative

On June 13, 2014, the Storm Prediction Center (SPC) noted the possibility of severe weather associated with potential mesoscale convective systems in the northern United States for June 16–18. However, the predictability of this event was too low for the SPC to designate areas at risk of severe weather. The following day, the SPC revised their forecasts, indicating a slight risk for severe activity for areas around the confluence of the Big Sioux and Missouri rivers two days before the eventual tornado outbreak. The development of a low-pressure area and increasing atmospheric instability were expected to be contributing factors. Forecasts remained relatively unchanged on June 15, though the probability for "significant severe weather" was predicted for a large area of northern Iowa and adjacent areas.

Event narrative

The morning of June 16 was marked only by isolated storms in the Nebraska area with only marginal severe weather. Beginning at around 0800 UTC, however, favorable conditions for severe weather, particularly for large hail, began to build across central Nebraska. Moisture from the Gulf of Mexico began to make its way into southern Nebraska and over Kansas, raising dew points over the region. In addition, the prevalence of altocumulus castellanus clouds was an indicator of additional severe weather later in the day. The flow of moisture into the region was further enhanced by an eastward progressing warm front, and at 0600 UTC on June 16, the SPC once again issued a slight risk for severe weather for the eastern halves of South Dakota, Nebraska, and extending eastward into the western Great Lakes region. This was followed shortly after by the day's first severe thunderstorm watch, issued for primarily eastern Nebraska in response to a developing line of supercells. An hour later, the SPC upgraded some areas previously under a slight risk for severe weather to a moderate risk as a result of continuously increasing moisture content and CAPE in the atmosphere. At 1613 UTC, the SPC issued the first of three public severe weather outlooks for the day, covering a region centered on Sioux City, Iowa. A Particularly Dangerous Situation tornado watch was issued later that afternoon.

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