packfan98
Moderator
You'll see lows from time-to-time jump from the windward side of the Apps to the eastern end in CAD events because the topographic blocking due to the mountains themselves (due to vorticity conservation compresses the column and deters cyclonic vorticity), and the strong low-level static stability in the CAD dome itself deters low-level cyclonic vorticity and acts as "effective topography", deflecting the track of the low pressure center around the mountains and CAD dome. Hope this makes sense haha!
Makes perfect sense. Thanks! The question is, will the low really end up on the windward side of the Apps like the Euro has????