Its curious to see where that European cold pool is coming from. The answer is (indirectly) Canada. It seems like a upper level trough drops across Europe around the time of the 2nd WAA. This then develops into a cold core cutoff low which intensifies at upper levels. It would seem the cold air then quickly intensifies, but through adiabatic expansion at high levels rather than any advection of cold air.
If this is the cold pool we are tapping into then its strength will be determined by the strength of the cold core low. The stronger it ends up being, the more divergence, the more expansional cooling and decrease in the uppers. So not really so much dependent on how cold the continent is?
Originally Posted by: Quantum