Ike was dealing with significant ENE'rly mid-level shear as it traversed across the north-central GOM. It wasn't enough to force weakening but after Cuba, Ike also had a large circulation. If you will recall, there was an intense westerly eyeband that could not wrap or stay wrapped for symmetry. The convection remained lopsided but intense enough to keep the large circulation chugging along as a big Category 2. Simply put, the battle between shear and thermal dynamics kept Ike at status quo all the way into landfall. Obviously surge was the issue and led us to a new parameter, IKE. Delta on the other hand should have a good window of much more favorable conditions to actually reattain major status while continuing to expand its convective envelope symmetrically up until moving over cooler SSTs and mid-level shear increases prior to landfall. Granted, the end result may be similar for landfall intensity, but Delta's maximum winds should get higher than Ike's maximum winds ever achieved in the GOM. This all being said, surge is going to be the biggest problem at the coast regardless if it maintains Category 3 or weakens to a 2 by landfall. Expansion and fetch will have already been achieved.