At the opposite end of the supercell scale is the Low Precipitation (LP) supercell. For years, storm chasers have observed LP storms in the Plains' states, usually in conjunction with a dry line or low pressure trough dividing dry, warm air to the west from very humid air to the east. These rotating storms typically are quite small and lacking in liquid rainfall content.

The radar echo rarely contains a pendant or hook, although the LP storm may have a tight reflectivity gradient at the southwest side. In many cases, the small size of the storm will not allow for adequate "beam filling", especially at moderate to long range from the radar. Therefore, the radar intensity of the small storm can be drastically underestimated.

Photograph by: Doswell

This northward view of an LP storm in western Oklahoma shows both the small size and the powerful nature of the updraft. This storm was shrinking to an even smaller size at this time, which is how most LP storms meet their demise. Note that the updraft tower is scarcely any wider than the wall cloud. The storm earlier produced golf ball size hail and, although it rotated vigorously, it did not produce any tornadoes.