It seems to me the inhibiting factor for development could be the broad circulation may have trouble tightening. This seems to be why the GFS has a very large hurricane, while the Euro has shown on several runs a broad area of low pressure that never develops despite reasonably favorable conditions.
I-85 is lava. Seems mid-level dry air should keep rain totals in check for the triad. The HRRR depicts this well, with around .5" and 1-2" just to our south.
Top gusts so far: 60 mph Wilmington, 67 mph Wrightsville beach, & a rather suspect looking 77 mph gust at sunny point. Meanwhile, even along the coastline only gusts in the mid 30s south of Bald Head.
Yeah I thought that was pretty well established a couple days ago, that a stronger storm could actually be enhanced by what on paper is shear. You think more of a net neutral impact overall though?
A bit concerning with respect to surge potential especially if this thing comes in a little stronger. Thankfully, for the most part, coastal LA does not build in the flood zones.
Looks like the GFS takes the energy from 90L across Mexico into the Pacific where it becomes a hurricane, making landfall in Mexico before crossing back into the Gulf and developing into a hurricane again.
Huge corrections from all models. Now many models have it slowing down prior to landfall which may give it an opportunity to go through ERC before landfall