MWatkins wrote:Brownsville radar might be having trouble getting all the way through those dense bands near the core. The opening is apparent from the Corpus long range...but they are getting a pretty good band on them as well.
Hopefully this has leveled off for now.
Note: If this were Miami the MIA (or now MFL) radar would have been down for 10 hours already. Props to NWS Brownsville for keeping the radar operational...
MW
I believe Dolly has already surpassed its peak intensity, which likely occurred around the time of the 8 a.m. CST advisory (or slightly before its release). A VDM indicated a minimum central pressure of ~964 mb after the advisory arrived, and the northern eyewall was still intact. I suspect that Dolly is clearly entraining dry low level air from the inland areas of Mexico and S Texas, which also occurred with Allen 1980, Emily 2005 (?), and other Texas TCs. As the TC appears to have stalled, more gradual weakening may occur prior to landfall. The winds at the surface have already dropped off slightly, in my view.
Sanibel, the fact is that Dean primarily impacted a rural area, and you apparently haven't seen Dean's impact on Mahahual.
Dolly is still a significant issue with the heavy precip and Cat 1 winds, though a weakening system is better than a deepening one. A weakening system may not bring the hurricane force winds/strong TS winds to locations further inland; however, in the area along the immediate coast, the impact remains identical. Cat 1 winds can certainly impact frail structures significantly.