All about that backside energy. If it trends stronger, we’ll see some tuckier solutions that may drive warmer air into eastern areas and push the ml goodies further inland.
I’m still trying to figure out what 8s allowing that subtle lifting out to get this further north. All I can see is some larger subtle downstream troughing that allows heights behind to lift a little more.
Throw up the GFS 500mb North Atlantic view on Tropical Tidbits and you can see what I am referring to, our exiting storm takes its time, meanwhile our next storm comes in like a heat sealing missile, only to hit a brick wall.
This storm will only appear slow because it’s slamming into the system that’s exiting us now. I don’t see this as a maturing coastal as it hits our latitude. That’ll be further SW of us in the mid Atlantic. Doesn’t mean we can’t have a sizable storm, I just don’t see a WCB combined with a CCB to produce those prolific totals.
Nope. Shitstreak halts this bowling ball in its tracks and the main s/w than has to undercut it while the backside energy has no where to go but carve itself underneath the main s/w, which than elongates the entire system.