Visible satellite imagery indicates that Ike may be dealing with some dry air entrainment issues, as you can see a wedge of drier air wrapping around from the west through the south and into the northeast portion of the storm. That wedge of drier air (implied by relatively darkness in the visible sat imagery) looks quite similar to Ivan before IVan made landfall. In any case, I have to imagine that Ike will continue to moisten its environment (especially considering its large size), so, with relatively low shear, conditions should become more conducive to significant intensification soon. It is a bit odd to see such low winds with such low pressure. For quite some time, RECON was only finding Cat 1 winds (latest VDM notes 93 kt max FL winds), which was a tad surprising given the <962 mb central pressure. Of course, the relatively large size of Ike is likely lessening the local pressure gradient (similar perturbation pressure as some Cat 2-3 storms, but spread out over a larger area = weaker PGF), but it's still pretty interesting nonetheless.
Can anyone explain the primary forces that dictate the size of hurricanes? I'm not a tropical cyclone guru by any means, but I haven't read much about why some storms are small vs. why some are large. I can only assume size is a function of storm maturity (i.e. how "old" is the storm?), intensity, and upper-level outflow / environment... I 've noticed that a lot of intense hurricanes can start our relatively small but grow rather quickly, with some lag time between intensification and physical growth.