Smurfwicked wrote:What is aggravating is people freaking out that it could possibly go into SWLA all the sudden? I think not! That area has been in the Hurricane watch all along! People in the watch should of already been prepared!
You speak wisely.
Moderator: S2k Moderators
Smurfwicked wrote:What is aggravating is people freaking out that it could possibly go into SWLA all the sudden? I think not! That area has been in the Hurricane watch all along! People in the watch should of already been prepared!
This means the NHC is using a 74% reduction factor from the 61kts FL winds. I wonder why they are using 74% instead of 80%-90%?cycloneye wrote:Winds up to 45kts at ATCF best track at 00.00 UTC:
dhweather wrote:Clint_TX wrote:Well I'm not sure about track, but it's forward speed has slowed, it's blocked to the north and its becoming better organized...what will keep this storm from becoming a strong Cat 1 or Cat 2?
I would like someone to explain why that won't happen.
1) Their is an extremely dry mass of air immediately to the north of Ed in central and southern Mississippi.
2) The flow of that dry air is to the west-southwest. Dry air and tropical cyclones don't mix together well, the dry air wins 99% of the time.
3) Ed is sitting in shallow water. As he churns up that shallow water and cools it off, he will cut his own lifeline if he sits there.
4) There is no significant convection on the western half of the storm, thus it is not symmetrical. Healthy, symmetrical cyclones intensify much faster than disorganized ones like Ed.
5) There's an upper level low over the Yucatan peninsula that is nudging Ed towards the North and is alos interfering with his outflow.
I would be surprised if he's anything more than a weak cat one tomorrow.
hwego7 wrote:This means the NHC is using a 74% reduction factor from the 61kts FL winds. I wonder why they are using 74% instead of 80%-90%?cycloneye wrote:Winds up to 45kts at ATCF best track at 00.00 UTC:
I personally think it is an illusion (but I could be wrong). The strongest band on radar looks to be rotating NW around the center, but the center itself still seems to be moving more W or WNW.KatDaddy wrote:Its looks to me move NW on the Lake Charles radar.
They had it at 40kts on the 7pm update so to bump the winds up 5kts they most certainly were using the 61kt FL wind data from recon.cheezyWXguy wrote:That was probably put out before those flight level winds were observed. Winds are likely around 50kt by now.
Smurfwicked wrote:What is aggravating is people freaking out that it could possibly go into SWLA all the sudden? I think not! That area has been in the Hurricane watch all along! People in the watch should of already been prepared!
Cape Verde wrote:I still don't see how Edouard hits Galveston/Houston by noon tomorrow. At 7 or 8 mph, it's still 24 hours away.
What am I missing?
hwego7 wrote:They had it at 40kts on the 7pm update so to bump the winds up 5kts they most certainly were using the 61kt FL wind data from recon.cheezyWXguy wrote:That was probably put out before those flight level winds were observed. Winds are likely around 50kt by now.
dhweather wrote:Clint_TX wrote:Well I'm not sure about track, but it's forward speed has slowed, it's blocked to the north and its becoming better organized...what will keep this storm from becoming a strong Cat 1 or Cat 2?
I would like someone to explain why that won't happen.
1) Their is an extremely dry mass of air immediately to the north of Ed in central and southern Mississippi.
2) The flow of that dry air is to the west-southwest. Dry air and tropical cyclones don't mix together well, the dry air wins 99% of the time.
3) Ed is sitting in shallow water. As he churns up that shallow water and cools it off, he will cut his own lifeline if he sits there.
4) There is no significant convection on the western half of the storm, thus it is not symmetrical. Healthy, symmetrical cyclones intensify much faster than disorganized ones like Ed.
5) There's an upper level low over the Yucatan peninsula that is nudging Ed towards the North and is alos interfering with his outflow.
I would be surprised if he's anything more than a weak cat one tomorrow.
cheezyWXguy wrote:hwego7 wrote:This means the NHC is using a 74% reduction factor from the 61kts FL winds. I wonder why they are using 74% instead of 80%-90%?cycloneye wrote:Winds up to 45kts at ATCF best track at 00.00 UTC:
That was probably put out before those flight level winds were observed. Winds are likely around 50kt by now.
MiamiensisWx wrote:dhweather wrote:1) Their is an extremely dry mass of air immediately to the north of Ed in central and southern Mississippi.
2) The flow of that dry air is to the west-southwest. Dry air and tropical cyclones don't mix together well, the dry air wins 99% of the time.
3) Ed is sitting in shallow water. As he churns up that shallow water and cools it off, he will cut his own lifeline if he sits there.
4) There is no significant convection on the western half of the storm, thus it is not symmetrical. Healthy, symmetrical cyclones intensify much faster than disorganized ones like Ed.
5) There's an upper level low over the Yucatan peninsula that is nudging Ed towards the North and is alos interfering with his outflow.
I would be surprised if he's anything more than a weak cat one tomorrow.
1. The dry air was an issue earlier, and I correctly implied that it would "stunt" Edouard's intensification to certain degrees. However, the dry air is much less significant than earlier. Check the local soundings and SKEW-T plots (such as Lake Charles, LA) as of 18Z and compare them to 12Z. The mid level moisture is increasing, while the dry air at the low levels within the boundary layer is mixing out now (at last). Earlier, convection failed to develop and sustain itself over the LLC; tonight is a different story. This TC is likely slowly intensifying now, unlike the situation throughout most of the day.
2. Respectfully, please see response to #1.
3. Remember that tropical cyclones rely on latent heat to support their development and intensification. Edouard is currently over very warm SSTs and recently passed over deep oceanic heat content within the western portion of the Gulf Loop Current. The 26 C isotherm is relatively deep in Edouard's vicinity as well. Note that Edouard will not pass over the cooler SSTs, which are located well SOUTH of Galveston. The near shore SSTs will be warmer in the portion of Gulf from slightly south of Galveston to the Golden Triangle and coast of SW Louisiana. Edouard will make landfall within this region over or slightly NE of the entrance to Galveston Bay. The strong convection and small inner core will aid more greater releases of latent heat, while the increasingly unstable boundary layer will aid more rapid ascent of parcels. With minimal shear and less ML dry air, this supports gradual intensification. Additionally, Edouard will not be crawling at Dolly's rate, and it definitely won't stall. Steering does NOT support a Dolly redux, so upwelling will likely not be a greater issue with Edouard as it moves into the shallower coastal waters. Edouard is a more compact system in terms of aereal extent than Dolly as well, for what it's worth.
4. Please consider the changing thermodynamic environment. A few hours can make a big difference, as we are observing in this case.
5. The upper low has been enhancing ventilation and divergence, as well as outflow. It will continue to aid Edouard in this case, especially as northerly shear has diminished within the past 24 hours. Edouard is now UNDER the H5-H85 ridging.
"It will only be a Cat 1 or weaker..."
Firstly, I personally expect a strong TS at landfall.
Secondly, are you implying that people should stop paying attention to it even as it intensifies?
Thanks...
Bailey1777 wrote:It looks on that sat. like the top and bottom are spinning at different speeds?
Users browsing this forum: No registered users and 5 guests