timNms wrote: Of course, the eyewall didn't come anywhere near us, tho.
That's a HUGE point. In most storms, the highest winds are very tightly packed near the eyewall (i.e. there's usually a rather significantly gradient in winds beyond the eyewall). Katrina's windfield expanded rapidly right before landfall as it weakened a little. Regardless, your proximity to the eyewall is very important. A lot of people go through think that a "typical" Cat 3 that hits 60 miles away means that they experienced Cat 3 winds. Nope, very unlikely.
I assume that model is based on a standard rate of decay / weakening. As would be expected, the faster the storm is moving, the more distance it travels inland before it weakens a certain amount (e.g. from a Cat 4 to a Cat 1). I don't think that means that strong inland winds aren't possible, but perhaps not likely. Individual thunderstorms may have enhanced downdrafts that may lead to higher-than-expected winds (there are plenty of storm-scale flows involved).