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Rapidly rotating wall cloud and attendant tail cloud is
observed beneath the forward flank updraft of the first severe storm about 3
miles northwest of Jefferson, IA. |
The wall cloud shrivels but is still spinning. Vigorous dirt
whirls can be seen beneath the wall cloud. This wall cloud soon becomes
completely undercut by outflow as the storm becomes linear and gusts out. |
A new supercell blossoms at the tail end of the
aforementioned convective line. This is our view of it's rear flank core to
our southwest as we drive west on CRE57 towards Cooper, Iowa. |
We penetrate the forward flank core near Cooper and get
pelted by 1 to 1.5" diameter stones. We drive south in search of larger
stones near the updraft but soon get deflected east by a reported "sherrifnado". |
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We emerge from the rear flank core and drive east to get a
better look at the "action area". The storm is strongly undercut with
outflow racing away from the storm to its south and east. However, as is so
typical of these "high precipitation" storms, a narrow channel of
potentially buoyant inflow air is "feeding" the updraft from the north and
northeast. This airs stream becomes saturated as it encounters the cold
outflow and a wall cloud forms. This wall cloud was observed to rotate quite
rapidly. |
The same wall cloud with a stubby tail cloud feeding it from
the north-northeast along the forward flank gust front. Note both in this
picture and the previous the dry air that has wrapped into the circulation,
causing the wall cloud to be partially front-lit. This is the rear flank
downdraft. |
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