Winter Weather, Dawson
- When
- January 21, 9:00 AM CST to 6:00 PM CST
- Where
- Dawson forecast zone
- Reported by
- Trained Spotter
- Coordinates
- 40.870, -99.820 (the zone’s center; the record gives no point)
A moisture-starved, weak low pressure system dropped narrow bands of 3 to 4 inches of snow over a few communities on this Tuesday. This event really evolved as two separate areas of snow.
Every event with a place to put it; 8 filed by county or forecast zone are drawn at its center, in a lighter ring. Tap one for its entry below.
Deaths and injuries are direct and indirect together, as the offices filed them. Damage is property and crops in the dollars of the year, not adjusted for inflation, and only where an office estimated it.
The episode as NWS GID wrote it up.
A moisture-starved, weak low pressure system dropped narrow bands of 3 to 4 inches of snow over a few communities on this Tuesday. This event really evolved as two separate areas of snow. During the early to mid morning hours, a very narrow southwest-northeast oriented band of snow developed from eastern Colorado across northwest Kansas into southwest Nebraska. By late morning, this band moved into south central Nebraska from Johnson Lake to Miller to Loup City. This band gradually progressed eastward across south central Nebraska between 10 AM and midnight. This band was only two counties wide, but at times, there was an embedded band of heavy snow that was much more narrow, well less than one county wide. As this band initially moved into south central Nebraska, it was nearly stationary for about 3 hours from Cambridge to Elwood to Overton to Amherst. These locations are where the greatest snow amounts fell in association with this band. Three to five inches of snow was reported, with a maximum of 6 inches estimated in Cambridge. The visibility was estimated as low as 1/16 mi in heavy snow at Overton and Amherst. As this band moved east, its forward progress limited accumulations to 1 to 2 inches, and even less than 1 inch in some places. This snow band developed within the upper-level trough. The other area of snow developed in the late morning hours from central Kansas into southeast Nebraska. This band was a bit wider and was a poorly-organized deformation band and it deposited 3 to 4 inches of snow over eastern Nuckolls, Thayer, and southern Fillmore counties. Throughout this event, the character of all the radar returns, from both areas of snow, was so poorly-organized that the snow bands exhibited a skeletal structure.
At the surface, a weak low pressure system emerged from Colorado and moved east through Kansas. This low never had a closed isobar. In the upper-levels a positively-tilted trough was over Colorado and New Mexico at daybreak. This trough advanced into Nebraska, Kansas and extreme western Texas by sunset. This was the primary trough over the CONUS, with a ridge over the eastern Pacific and a ridge along the East Coast.
The national radar mosaic for the moment the first event began.
8 winter weather. Local standard time, as filed.
After NWS Directive 10-1605, the rules offices file Storm Data by.
Every storm in Nebraska in 2019Every state in 2019This day in weather historyWarnings in Nebraska, January 2019
NOAA National Centers for Environmental Information, Storm Events Database, compiled from the National Weather Service’s monthly Storm Data. Complete through 2026-06; NCEI adds each month about 75 days after it ends and revises past years a few times a year. Rebuilt 2026-10-01. Each event’s entry at NCEI: 798983, 798984, 798985, 798986, 798987, 798988, 798989, 798990.