Justin - sorry you just got in... We already noted that on page 1 of this thread (actually, I posted that information.)
NHC said sustained winds were 85mph with gusts to 110mph. If you can find ANY evidence of anything CLOSE to that, I will bow to your clear data.
I don't know why people try to discredit hard data with "I think"s. Meteorology is at its core a science, and science requires evidence. All evidence shows that the storm did not cross the Texas coast with 85mph sustained winds, and it also shows that the storm did not continue into LA with 65mph winds. Yet that's what NHC said, even as the observations proved otherwise...
I think a little perspective is needed here. The reconnaissance aircraft in Humberto at landfall fixed the center at 29 degrees 32 minutes North 94 degrees 21 minutes West. At 29 degrees 32 minutes North 94 degrees 11 minutes west - 9 nautical miles to the east - it measured a 850 mb flight-level wind of 98 kt. At 29 degrees 38 minutes North 93 degrees 57 minutes West - 14 nautical miles father to the east-northeast - the flight-level winds dropped below 65 kt. The surface winds probably dropped below 65 kt before then.
The only surface station on the coast in that area is the Sea Rim State Park C-MAN station at 29 degrees 40 minutes North 94 degrees 3 minutes west, which reported two 10-minute average winds of 60 kt. Now, we've not had the time to analyze the data in detail, but I would say there is a possibility the strongest winds passed just west of that station. Hopefully a detailed study of the WSR-88D winds will tell us if that was actually the case.
Now, a few miles doesn't sound like much. But in a tight-cored system such as Humberto a few miles can make a tremendous difference in the experienced winds. The flight-level winds in Humberto decreased about 10 kt over a 5 nautical mile distance out from the maximum measured wind, while in Wilma (an extreme example) the flight-level winds decreased about
70 kt over a 5 nautical mile distance out from the maximum measured wind.
The eye passed over the Beaumont airport, so the eyewall and the radius of maximum winds passed over the station. However, the strongest winds in the storm at the time could have been in the part of the eyewall that did not pass over the station - possibly off to the east. Radar data and damage surveys may tell us more about that.
As for after landfall, I was the duty hurricane specialist during that time. I didn't get any core surface wind observations between Beaumont and Alexandria, so I was relying mainly on WSR-88D data. (The winds in Lake Charles, for example, were probably not representative of the core winds.) Do you have any such observations that were taken in the radius of maximum winds? If so, could you please pass them along for our post-analysis?
We'll be doing some extensive post-analysis of this storm before we settle on a final set of intensities.
Jack Beven