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Hurricane Beryl Tropical Cyclone Update
NWS National Hurricane Center Miami FL AL022024
1100 PM CDT Sun Jul 7 2024
...BERYL IS AGAIN A HURRICANE...
Data from the National Weather Service Doppler radar near Houston,
Texas, and reports from an Air Force Reserve Hurricane Hunter
aircraft indicate that Beryl's maximum sustained winds have
increased to near 75 mph (120 km/h). Based on these data, Beryl is
upgraded to a hurricane. Additional strengthening is expected
before landfall on the Texas coast.
NOAA buoy 42019 recently reported sustained winds of 60 mph
(97 km/h) and a wind gust of 74 mph (119 km/h). The buoy also
reported a pressure of 992.2 mb (29.30 inches).
Major power problems persist in Houston. 460,000 customers without power, which is likely easily >1 million persons. In the midst of summer heat, this is a serious problem, especially for the unhoused, the elderly and the disabled.
Major power problems persist in Houston. 460,000 customers without power, which is likely easily >1 million persons. In the midst of summer heat, this is a serious problem, especially for the unhoused, the elderly and the disabled.
Yeah, I've heard a few folks say the Houston heat is just something else. Can't imagine trying to do it without any power right now.I've lived in many places, and having lived in Houston during a summer while working outdoors I can tell you that it's the closest to hell on earth that I've ever experienced. At 6AM local it's 90F+ and 90%+ humidity and then it gets worse from there. I was young used to working outside in summers but that was almost more than I could take. It would likely kill me to try it now.
Carriacou was also in the northern eyewall, where the winds would have been stronger than in the southern eyewall. That damage is really intense though; Beryl’s central pressure in the high 930’s at the point of impact on Carriacou, so I’m still a little confused as to why the intensity of the winds was so comparable to high end C5’s with pressures below 910 mb.After looking over at everything regarding wind damage in the windward islands, I can confidently say cat5 winds, (even high end) occurred in Carriacou, Petite Martinique, and especially Union Island.
I’ll go as far to say it was just as bad in Irma, even though there’s no evidence that Beryl was a cat5 at landfall. Although this can easily be explained by the mountains in which the infrastructure is built on.
Without further a do, here’s the physical evidence, with vegetation. In the first photo, all vegetation has been 100% denuded, regardless of the type, even the palm trees were reduced to match sticks.
In the second photo, you can even see moderate debarking on some of the use to be trees. Especially the third photo, the vegetation has that classic “bleached/burned” look, a phenomena that I’ve seen exclusive to only high end cat5 winds.
The fourth photo is the most impressive to me, as the damage here to vegetation is something I haven’t seen in many ef4 rated tornadoes. Just a slew of granulated pieces of debarked branches and trees that look like they went through a nuclear blast.
The last photo more or less shows the same thing, and that even trees with large trunks and branches were no match whatsoever.
I’ve already shown you guys the structural damage in earlier photos, mainly with the surprising amount of reinforced concrete buildings destroyed.
I’m telling you, there are way, waaay more, to the point that I’ve haven’t seen so many destroyed since Irma and even Haiyan. There’s so many of these destroyed structures it’s pointless to show all of them.
It’s to the point where the only explanation I can think of is that this storm must of had unusually high gust even for its strength, well into the 200mph range. Which is a phenomenon that can occur in rapidly strengthening hurricanes combined with mountainous terrain.
Which is the only explanation that makes sense other than saying that Beryl was a straight up 160knot storm. Because not even Maria in Dominic and Puerto Rico did anything like this despite supposedly being the stronger storm.
The pressure can be explained by small size and background sea level pressures. Smaller storms have much tighter pressure gradients, especially if they’re being superimposed on by a ridge.Carriacou was also in the northern eyewall, where the winds would have been stronger than in the southern eyewall. That damage is really intense though; Beryl’s central pressure in the high 930’s at the point of impact on Carriacou, so I’m still a little confused as to why the intensity of the winds was so comparable to high end C5’s with pressures below 910 mb.