rburrel2
Member
		Here you can see how the euro goes bonkers with adiabatic cooling at 850mb from the SE flow lifting over the surface wedge/mountains... That's all thanks to a robust shortwave going neutral tilt over the MS river.  On the other hand, the gfs has a faster/weaker/flatter wave and keeps winds out of the SW at 850mb as the storm passes over so no cooling at 850mb.

				
			

 
				 
 
		 
 
		 
 
		
 
	 
	
 
	 
 
		 
 
		 
 
		 
 
		 
 
		
 
 
		 
 
		 
 
		