About 3-4 minutes after the initial wall cloud had produced a possible tornado. this more outflow dominated base feature developed.
At this stage the area of rotation was not quite as tight and produced this more elongated shaped linear outflow jet.
It was not long after this feature dissipated that the entire area began to get rain wrapped and the whole storm rapidly began to dissipate.
Interestinly enough however, to the immediate west of this storm a line of small multi=cell storm complexes quickly developed after the dissipation of the first storm, and moved rapidly to the south-east direction.
Some large hail and destructive straight line winds seemed likely based on radar signatures depicted by this storm. but was once again quite short lived.
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ZoeIzAwsum 2 years ago