steph
Well-known member
Yep, it's been a few wild days for severe weather in Central Europe. Normally, the one forming due to a stationary front would be of the landspout variety, but yes...while I wouldn't go as far as saying they form from the ground up, it's almost always stuff in the lower-most inflow layers in surface-based storms that kicks up the feedback loops leading to tornadic formation. I've been a storm spotter for over 10 years now, seen a few funnels, but I still find it hard to wrap my head around the whole thing.
Even with supercells, having a deep rotating updraft and the RFD kicking in surely helps, but even so, not all produce even if all the conditions are met. Packs of more buoyant air, as well as local air currents producing low level shear due to the topography might form the initial vortex, which then gets picked up and stretched, or integrated, in the bigger circulation.
Even with supercells, having a deep rotating updraft and the RFD kicking in surely helps, but even so, not all produce even if all the conditions are met. Packs of more buoyant air, as well as local air currents producing low level shear due to the topography might form the initial vortex, which then gets picked up and stretched, or integrated, in the bigger circulation.
