NBAcentel
Member
That and interaction with a phasing upper level low/trough will aid in a extra-tropical transition which should keep strong winds going, while this isn’t a sting jet, the processes aren’t far apart, soundings in that intense low level jet show drying in the upper levels, but also try to creep in some drying more into the mid to lower levels, any light precip falling in this bit of dry air aloft would only help to drag down those winds, or clearing would also do the trickThere’s some big differences with this though. Most storms that hit N.C. are weakening at landfall while this storm has intensified right up to landfall. Also this storm is moving extremely fast which aids in bringing stronger winds to the surface.



