Estofex gaat ook mee, al zijn ze vergeten de Benelux te noemen:
"...Southern UK...
Remaining instability becomes shallower at the advance of warmer air aloft, but GFS shows considerable buoyancy below 700 hPa. In minimal flow conditions, the setup could be favourable to produce a few spout-type tornadoes/funnels, especially where convergence and vorticity organise locally (if LL instability indeed realises)
Other areas where more isolated spout-type tornadoes may form are the TSTMS area over Germany, and southern Sweden."
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