INVEST 92L SE GOM Sat Pics,Models,Analysis
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- vacanechaser
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however, remember shear is not shear if it is moving in the same direction as the shear...
Jesse V. Bass III
http://www.vastormphoto.com
Hurricane Intercept Research Team
Jesse V. Bass III
http://www.vastormphoto.com
Hurricane Intercept Research Team
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vacanechaser wrote:however, remember shear is not shear if it is moving in the same direction as the shear...
Jesse V. Bass III
http://www.vastormphoto.com
Hurricane Intercept Research Team
Interesting point Jesse. What if it is moving in the same direction as the shear but at a very slow pace?
<RICKY>
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- vacanechaser
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i would think it would rip it up... but you would think it would move faster with the shear...i guess...lol
Jesse V. Bass III
http://www.vastormphoto.com
Hurricane Intercept Research Team
Jesse V. Bass III
http://www.vastormphoto.com
Hurricane Intercept Research Team
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- windstorm99
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- Noles2006
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lothian wrote:Nole2006,
do you think we will see any rain this weekend?
NWS Tallahassee doesn't really think so... I think the highest POP in town for this weekend was 30, so it doesn't look too good.
Even with the Regional this weekend, I still wouldn't mind a lot of rain. Right now, rain ranks a little higher in importance (not by much, though!).
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- seaswing
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Noles2006 wrote:Frank2 wrote:Yes - hopefully just rain for the gators (the kind in the water - not on the field)...
Yes, because there won't be any gators playing on any (baseball) field anywhere this weekend...
Yeah but they will certainly be on the field (football) in August...watch out Noles'!

Seas
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I think this system is coming together quite nicely. Looking at the last visible loop, I think we very well may have an upgrade to Depression just as the system nears the west tip of Cuba. Here is the latest loop. Note overall improvement in organization.
http://www.ssd.noaa.gov./goes/east/gmex/loop-vis.html
http://www.ssd.noaa.gov./goes/east/gmex/loop-vis.html
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- AJC3
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In reality, if it wasn't for the shear, this system wouldn't be firing off convection like it's doing at the moment, and you wouldn't have the mechanism for generating the pressure falls that are occuring over the area.
http://www.rap.ucar.edu/weather/upper/upaCNTR_250.gif
http://cimss.ssec.wisc.edu/tropic/real- ... gjava.html
This is all related to the trough that's dipping into the GOMEX. It's actually increasing upper level winds just to the north and creating a healthy increase in the divergent shear over the northwest Caribbean. What you have going on is mostly jet-forced ascent, a baroclinic (non-tropical) process that is mostly responsible for the low spinning up. All the convection is on the east side of the storm, which really doesnt bode well for a system to become warm core, rather all that latent heat being released on the east side of the system would likely serve to strenghten the warm sector.
Given the mid to upper level pattern over the GOMEX, I can't see this system ever becoming a true TC. Either partly (i.e. a hybrid) to mostly a baroclinic low seems more likely to me.
http://www.rap.ucar.edu/weather/upper/upaCNTR_250.gif
http://cimss.ssec.wisc.edu/tropic/real- ... gjava.html
This is all related to the trough that's dipping into the GOMEX. It's actually increasing upper level winds just to the north and creating a healthy increase in the divergent shear over the northwest Caribbean. What you have going on is mostly jet-forced ascent, a baroclinic (non-tropical) process that is mostly responsible for the low spinning up. All the convection is on the east side of the storm, which really doesnt bode well for a system to become warm core, rather all that latent heat being released on the east side of the system would likely serve to strenghten the warm sector.
Given the mid to upper level pattern over the GOMEX, I can't see this system ever becoming a true TC. Either partly (i.e. a hybrid) to mostly a baroclinic low seems more likely to me.
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- cycloneye
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AJC3 wrote:In reality, if it wasn't for the shear, this system wouldn't be firing off convection like it's doing at the moment, and you wouldn't have the mechanism for generating the pressure falls that are occuring over the area.
http://www.rap.ucar.edu/weather/upper/upaCNTR_250.gif
http://cimss.ssec.wisc.edu/tropic/real- ... gjava.html
This is all related to the trough that's dipping into the GOMEX. It's actually increasing upper level winds just to the north and creating a healthy increase in the divergent shear over the northwest Caribbean. What you have going on is mostly jet-forced ascent, a baroclinic (non-tropical) process that is mostly responsible for the low spinning up. All the convection is on the east side of the storm, which really doesnt bode well for a system to become warm core, rather all that latent heat being released on the east side of the system would likely serve to strenghten the warm sector.
Given the mid to upper level pattern over the GOMEX, I can't see this system ever becoming a true TC. Either partly (i.e. a hybrid) to mostly a baroclinic low seems more likely to me.
Tony,the most important thing that this system will do is to pour rain where it's badly needed.Hopefully many areas in the Florida Penninsula and SE U.S. gets it.
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Visit the Caribbean-Central America Weather Thread where you can find at first post web cams,radars
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- AJC3
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cycloneye wrote:AJC3 wrote:In reality, if it wasn't for the shear, this system wouldn't be firing off convection like it's doing at the moment, and you wouldn't have the mechanism for generating the pressure falls that are occuring over the area.
http://www.rap.ucar.edu/weather/upper/upaCNTR_250.gif
http://cimss.ssec.wisc.edu/tropic/real- ... gjava.html
This is all related to the trough that's dipping into the GOMEX. It's actually increasing upper level winds just to the north and creating a healthy increase in the divergent shear over the northwest Caribbean. What you have going on is mostly jet-forced ascent, a baroclinic (non-tropical) process that is mostly responsible for the low spinning up. All the convection is on the east side of the storm, which really doesnt bode well for a system to become warm core, rather all that latent heat being released on the east side of the system would likely serve to strenghten the warm sector.
Given the mid to upper level pattern over the GOMEX, I can't see this system ever becoming a true TC. Either partly (i.e. a hybrid) to mostly a baroclinic low seems more likely to me.
Tony,the most important thing that this system will do is to pour rain where it's badly needed.Hopefully many areas in the Florida Penninsula and SE U.S. gets it.
Absolutely, Luis. I was simply couching my discussion in terms of actual TC formation, which to me is looking questionable. The model consensus of a sloppy, sheared, convectively "right-sided" low pressure system moving up into the eastern GOMEX and then across the northern half of Florida is something I've alluded to in previous posts, and would be just what our CWA needs.
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- Incident_MET
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