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SummaryMonitoring & Reporting | Safety

A series of thunderstorms popped up across the state today, one of these thunderstorms even caused a landspout tornado to form on Casper Mountain! The atmosphere is not primed for tornadoes today, and no rotation was evident on radar, so what happened?

Landspouts form when pre-existing horizontal circulations are stretched and tilted upward by a developing thunderstorm updraft. As with gustnadoes, landspouts do not usually form from mesocyclones or supercells. In fact, a large number of landspouts are observed in association with simple developing showers, often before precipitation is visible on radar. However, storm interceptors have noted the presence of landspouts in conjunction with supercell thunderstorms, sometimes at the same time as, but in a different part of the storm than a supercell tornado. Landspouts are usually visible, unlike gustnadoes, and most have a narrow, rope-like condensation funnel extending from cloud base to the ground. Wall clouds are not usually observed with landspouts, and these tornadoes are typically short-lived and weak. Damage associated with landspouts is usually not noted, but it can be significant with damage in the F1 category possible with wind speeds as high as 110mph possible.

Landspout tornadoes are typically not visible on radar, like their traditional supercell counterparts and usually go unwarned for that reason.

 We have not recieved any reports of damage from this tornado, but we have received several pictures! Thank you to those of you that have sent them in. If you have a photo that you would like to share, please post it on our Facebook page or send it to cr.wxriw@noaa.gov

 

Supplemental Images - Click Thumbnails To Enlarge
Radar Velocity at the Time of the Tornado
Velocity Image of a "Real" Supercell Tornado
May 6 Set-up
 

 

Image By LightAlive Photography
 
Image by Shawn Covert

If you have additional photos or video of this storm, please share them with us!
 

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