1992 Andrew report update
Moderator: S2k Moderators
Forum rules
The posts in this forum are NOT official forecasts and should not be used as such. They are just the opinion of the poster and may or may not be backed by sound meteorological data. They are NOT endorsed by any professional institution or STORM2K. For official information, please refer to products from the National Hurricane Center and National Weather Service.
- Tampa Bay Hurricane
- Category 5
- Posts: 5597
- Age: 37
- Joined: Fri Jul 22, 2005 7:54 pm
- Location: St. Petersburg, FL
- WaitingForSiren
- Category 1
- Posts: 383
- Joined: Sun Jan 08, 2006 12:58 pm
- Location: Minneapolis,Minnesota
- Contact:
I dont really get all this talk about only Cat 3 storms making landfall in the GOM when Camille was a cat 5. Katrina was a Cat 4, possibly even a 5, wasnt she?
I think as the dynamics change and the water heat content changes, along with eyewall cycles each year it will be varied. There is no such thing as a spot where the hurricane will always weaken, unless of course there is cold water there.
I think as the dynamics change and the water heat content changes, along with eyewall cycles each year it will be varied. There is no such thing as a spot where the hurricane will always weaken, unless of course there is cold water there.
0 likes
- LSU2001
- S2K Supporter
- Posts: 1711
- Age: 57
- Joined: Sat Sep 11, 2004 11:01 pm
- Location: Cut Off, Louisiana
Derek,
While I agree with your analysis of downgrading storms such as camile and Katrina, I disagree about the waters just offshore being cold or cool just below the surface. I have scuba dived offshore of La for years and in the summer and in the heart of hurricane season the water is bathtub warm down to at least 100 ft. I guess I will have to bring down a thermometer on my next trip to really find out what the temp below the surface is. Now I realize that I am talking only about 45-50 miles offshore but I find it hard to believe that the gulf cools off that much further out.
Tim
While I agree with your analysis of downgrading storms such as camile and Katrina, I disagree about the waters just offshore being cold or cool just below the surface. I have scuba dived offshore of La for years and in the summer and in the heart of hurricane season the water is bathtub warm down to at least 100 ft. I guess I will have to bring down a thermometer on my next trip to really find out what the temp below the surface is. Now I realize that I am talking only about 45-50 miles offshore but I find it hard to believe that the gulf cools off that much further out.
Tim
0 likes
Personal Forecast Disclaimer:
The posts in this forum are NOT official forecast and should not be used as such. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
The posts in this forum are NOT official forecast and should not be used as such. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
I believe that the waters are churned up more than 100 feet. I believe that the first 200 feet is what really matters
Now, in the Caribbean, the 26 degree isotherm is several hundred meters below the surface. The cold waters are never upwelled there, even if a slow poke like Wilma or Mitch sits in the same place for days. They never ran into upwelling issues
Now, in the Caribbean, the 26 degree isotherm is several hundred meters below the surface. The cold waters are never upwelled there, even if a slow poke like Wilma or Mitch sits in the same place for days. They never ran into upwelling issues
0 likes
- LSU2001
- S2K Supporter
- Posts: 1711
- Age: 57
- Joined: Sat Sep 11, 2004 11:01 pm
- Location: Cut Off, Louisiana
Thanks for the clarification. I can see the upwelling causing rapid cooling of the water. I also believe that an influx of dry air from texas and southwest US cause a lot of the weakening that we see in these storms. If you look at the radar loop of Katrina you will see the dry air enter the south west part of the storm and that part of the eyewall seems to simply collapse. It later partially reforms but the weakening is quite evident.
Tim
Tim
0 likes
Personal Forecast Disclaimer:
The posts in this forum are NOT official forecast and should not be used as such. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
The posts in this forum are NOT official forecast and should not be used as such. They are NOT endorsed by any professional institution or storm2k.org. For official information, please refer to the NHC and NWS products.
- Pearl River
- S2K Supporter
- Posts: 825
- Age: 66
- Joined: Fri Dec 09, 2005 6:07 pm
- Location: SELa
- WaitingForSiren
- Category 1
- Posts: 383
- Joined: Sun Jan 08, 2006 12:58 pm
- Location: Minneapolis,Minnesota
- Contact:
- MGC
- S2K Supporter
- Posts: 5907
- Joined: Sun Mar 23, 2003 9:05 pm
- Location: Pass Christian MS, or what is left.
Since the NHC don't have the tools to look back at Camille, how are they (NHC) going to reanalyse Camille? They don't have GPS sondes, no SFMR, no doppler radar. Nothing but hours old recon report and 909mb pressure observed at landfall. Since the pressure was up only a few mb there is evidence that Camile didn't have a eyewall replacement like Katrina did. The GOM was quite warm since 1969 was a very hot year along the gulf coast. That lead to very warm SST and Camille passed over the loop current so she had plenty of warm water. She had a small eye on the order of 8NM in diameter. Do the math, 909mb and 8NM eye. What does your formula crank out? Just curious......MGC
0 likes
Not only were Katrina's sustained winds no higher than Cat 3, the surge, except for an *extremely* small area of coastline, was Cat 3 as well. The storm tide included approx two feet of high tide on top of the surge along most areas of the MS Gulf Coast, and for the few areas that received slighly higher surge, it was a moot point, because they were all right along the shoreline, and were hit with large battering waves on top of the surge.
Because the MS Gulf Coast is a tidal plain, a Cat 3 surge can go very far inland. The area of Cat 3 surge was so extensive -- unprecendented, really -- because Katrina was such a large storm.
I believe Katrina and Camille to be similar in many ways, and that the more detailed understanding we have of Katrina can also lead to a better understanding of Camille's structure. I suspect Camille may have also had a degradation of winds to the west and a broadening of the wind gradient to the east, because of the widespread but not severe wind damage that occured in Pascagoula. And if you remember the roadway sections of the Ocean Springs Biloxi Bay bridge were moved around with Camille to where you could just barely drive across it with the help of plywood or whatever it was they laid down between some of the sections, just not knocked clear off the supports as with Katrina, and likely the difference in height of the surge, and the larger waves from Katrina, made that difference, but it is probably not as large a difference as you might think.
Because the MS Gulf Coast is a tidal plain, a Cat 3 surge can go very far inland. The area of Cat 3 surge was so extensive -- unprecendented, really -- because Katrina was such a large storm.
I believe Katrina and Camille to be similar in many ways, and that the more detailed understanding we have of Katrina can also lead to a better understanding of Camille's structure. I suspect Camille may have also had a degradation of winds to the west and a broadening of the wind gradient to the east, because of the widespread but not severe wind damage that occured in Pascagoula. And if you remember the roadway sections of the Ocean Springs Biloxi Bay bridge were moved around with Camille to where you could just barely drive across it with the help of plywood or whatever it was they laid down between some of the sections, just not knocked clear off the supports as with Katrina, and likely the difference in height of the surge, and the larger waves from Katrina, made that difference, but it is probably not as large a difference as you might think.
Last edited by Margie on Tue Jan 10, 2006 12:44 pm, edited 1 time in total.
0 likes
WaitingForSiren wrote:Katrina was only a three? No way, it had barometric pressure of cat 5 storm and judging by the damage theres NO WAY that thing was a three.
From the post TC report on Katrina:
"The relatively weak winds in Katrina for such a low pressure are the result of the broadening pressure field on 29 August that spread the pressure gradient over a much larger than average distance from the center, as confirmed by both surface and aircraft observations. The generally weakening convection likely also reduced momentum mixing down to the surface, contributing to surface winds being less than what the usual 90% adjustment from flight level winds would dictate. Katrina exemplifies that there is not simply a direct one-to-one relationship between the central pressure and the maximum sustained winds in a hurricane."
Also, the wind damage was consistent with a Cat 3.
Katrina should be remembered. This is what a Cat 3 does! This is the level of damage that can occur with a Cat 3 (mostly surge damage rather than wind damage, in a tidal plain). There is no need to 'supersize' hurricanes in your mind to Cat 4 or 5, as a way to justify the damage. A large, high-end Cat 3...bad enough.
0 likes
- Pearl River
- S2K Supporter
- Posts: 825
- Age: 66
- Joined: Fri Dec 09, 2005 6:07 pm
- Location: SELa
60 miles would make Camielle roughly the size of Ivan then.
was the 160 gust in Slidell from Camielle or Katrina? And if Camielle, what type of anamometer. If its hot wire, you may want to multiply by .65 to get the real wind speeds, as that was the reduction needed to get a real gust from keesler AFB from Georges, as its hot wire anamometer measured a gust to 172 m.p.h., when the real gust was about 123 (explains the 229 gust from Camielle, may have been closer to 140)
was the 160 gust in Slidell from Camielle or Katrina? And if Camielle, what type of anamometer. If its hot wire, you may want to multiply by .65 to get the real wind speeds, as that was the reduction needed to get a real gust from keesler AFB from Georges, as its hot wire anamometer measured a gust to 172 m.p.h., when the real gust was about 123 (explains the 229 gust from Camielle, may have been closer to 140)
0 likes
Derek Ortt wrote:60 miles would make Camielle roughly the size of Ivan then.
was the 160 gust in Slidell from Camielle or Katrina? And if Camielle, what type of anamometer. If its hot wire, you may want to multiply by .65 to get the real wind speeds, as that was the reduction needed to get a real gust from keesler AFB from Georges, as its hot wire anamometer measured a gust to 172 m.p.h., when the real gust was about 123 (explains the 229 gust from Camielle, may have been closer to 140)
Wats the inland gust ratio that Alskahuna always talks about? If I remember correctly, he said something like a 100 mph hurricane can produce 150 mph gusts over land due to the friction.
0 likes
Who is online
Users browsing this forum: jconsor, WeatherCat and 64 guests