Yesterday I took a look to the maps and it seemed that there was a low pressure in southern Nebraska. Today things have changed a little with less low level back winds even though it remains a good line of convergence in Nebraska. Thermodynamic parameters remains so good with more than 3000 of Cape spread in a huge zone.
So far there's only a thing that I don't like: the disposition of storm motion vectors and 0-6km shear vectors that appear to be more favorable for linear convection.![]()
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Andrea Griffa
www.cacciatoriditornado.it
www.tornado-tour.com
Coautore del libro "temporali e tornado"
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