Sanibel wrote:You should be careful about Franklin Fujiwaring off a ULL. If Franklin reacts to a ULL it will be incidental instead of controlling. The dominating steering feature is the Atlantic synoptic, not the ULL.
Normally, you'd think so, but as I observe Franklin, it's not being dragged up by the zippin'-along northward-moving flow (on the west side of the Bermuda high) just to its east; instead, the TS is just sitting where it is and spitting off successions of outflow boundries to the northeast. Meanwhile, the surface front has cleared the Carolina outer-banks, and winds are now out of the north and northeast there.
(I thought the Florida feature was a tongue of high pressure) (It's probably a surface High)
Well, you can have surface high pressure associated with an upper-low (the feature clearly is an ULL on WV).
Predictaguesstimate: The short-wave trough (and associated mid-level easterlies) will rapidly exit the east-coast, leaving a lingering horizontally-draped front off-shore; this front will quickly modify and wash out (it has already done so on land, where it can no longer be discerned in the southeastern states. In approx 24-36hrs, the front will be completely dissolved, leaving behind Franklin on the south side of a strengthening ridge; the is an good chance Franklin will be a hurricane by this time. In about two days, west-southwest-ward movement should take Franklin near or over Florida.