Robert Dewey
EF5
Since this really isn't a forecast, I'm gonna start a TALK thread...
SPC doesn't even have a SLGT out for the region on MON. This is probably due to the fact that northwest flow events are relatively hard to forecast - you have timing issues, whether or not any previous days convection will interfere, low level moisture return, etc..
Personally though, I would have gone SLGT. Whenever I see instability greater than (MLCAPE) 2000J/KG, and a +50knt jet max around 500mb - it should at least warrant a SLGT risk. I see the IWX went ahead and put a SLGT risk in their local HWO product, which seems reasonable to me. But again, major drawbacks, at least between the 00Z NAM and the 06Z NAM are timing. GFS still has somewhat of a convective look to it, but the development of a wave along the front is completely possible, though probably not to the extent the 06Z GFS shows. That would end up enhancing low level directional shear quite a bit, but could also disrupt moisture flow by firing all of the convection a little too far south for my liking.
SPC doesn't even have a SLGT out for the region on MON. This is probably due to the fact that northwest flow events are relatively hard to forecast - you have timing issues, whether or not any previous days convection will interfere, low level moisture return, etc..
Personally though, I would have gone SLGT. Whenever I see instability greater than (MLCAPE) 2000J/KG, and a +50knt jet max around 500mb - it should at least warrant a SLGT risk. I see the IWX went ahead and put a SLGT risk in their local HWO product, which seems reasonable to me. But again, major drawbacks, at least between the 00Z NAM and the 06Z NAM are timing. GFS still has somewhat of a convective look to it, but the development of a wave along the front is completely possible, though probably not to the extent the 06Z GFS shows. That would end up enhancing low level directional shear quite a bit, but could also disrupt moisture flow by firing all of the convection a little too far south for my liking.