rburrel2
Member
One negative is it seems this storm will rely on cad building in during the storm… that’s typically always delayed by several hours from whatever the models show, and can bust on the too cold side. Really too early to worry much about details like that though. What we really need is for tpv to really rotate in ahead of the storm. Models are all over the place on how it evolves but we really need a lobe to dive hard out ahead of the storm to push the boundary south and set up the confluence.
Outside of that, we really need the shortwave to trend slower and stronger, imo. Slower allows potential confluence to build in more… and stronger increases that gradient… if we get it strong enough to have a Miller B look like the euro shows it turns 85-900mb winds to out of the southeast which really sets off adiabatic cooling against the mountains with the strong wedge underneath.
Outside of that, we really need the shortwave to trend slower and stronger, imo. Slower allows potential confluence to build in more… and stronger increases that gradient… if we get it strong enough to have a Miller B look like the euro shows it turns 85-900mb winds to out of the southeast which really sets off adiabatic cooling against the mountains with the strong wedge underneath.