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Originally posted by Cloudsinthesky
Stifled reports from across the Gulf States region
Don’t be fooled by the media and the Government when Alex only turns out to be a category I or II and even if it just stays a tropical depression. The results will be the same, a toxic rain being dumped inland.
Actually all of the folks I've seen interviewed on this say that a Hurricane might be the best thing for the dilution of these things.
Originally posted by Granite
reply to post by Cloudsinthesky
You are spreading fear and ignorance.
I checked my sources at NOAA just now and there is nothing developed or nearly developed as a tropical storm level.
Go back to your cave...
Originally posted by getreadyalready
Originally posted by Granite
reply to post by Cloudsinthesky
You are spreading fear and ignorance.
I checked my sources at NOAA just now and there is nothing developed or nearly developed as a tropical storm level.
Go back to your cave...
Now, run along back to your so-called sources, and check a little better, because everybody else found it with no problem!
ZCZC MIATWOAT ALL
TTAA00 KNHC DDHHMM
TROPICAL WEATHER OUTLOOK
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
200 PM EDT TUE JUN 22 2010
FOR THE NORTH ATLANTIC...CARIBBEAN SEA AND THE GULF OF MEXICO...
1. A TROPICAL WAVE OVER THE CENTRAL CARIBBEAN SEA HAS BECOME LESS
ORGANIZED TODAY. SHOWERS AND THUNDERSTORMS ASSOCIATED WITH THE
WAVE WILL LIKELY SPREAD ACROSS PORTIONS OF THE DOMINICAN
REPUBLIC...HAITI...JAMAICA...AND EASTERN CUBA DURING THE NEXT DAY
OR SO. THERE IS A LOW CHANCE...20 PERCENT...OF THIS SYSTEM
BECOMING A TROPICAL CYCLONE DURING THE NEXT 48 HOURS. HOWEVER...
ENVIRONMENTAL CONDITIONS ARE EXPECTED TO BECOME MORE CONDUCIVE FOR
SLOW DEVELOPMENT OF THIS SYSTEM OVER THE NEXT SEVERAL DAYS AS IT
MOVES WEST-NORTHWESTWARD AT ABOUT 10 MPH.
Wind: 30 MPH — Location: 15.5 74.4W — Movement: W
This area of disturbed weather has the potential for tropical development.
Your Latest Florida Weather Information
Hi everybody. We are now watching invest 93 with care. Invest 93 is now a broad area of cloudiness that is beginning to show some signs of development. Right now, the upper level winds are not really favorable for development but that is expected to change over the next couple of days. A depression could form in another day or two. Initially, the model runs were keeping the invest well to our south but the new models are showing more of a course east of the Bahamas. Because of this model shift, it is definitely worth watching. Here are the latest model runs. A recon will investigate the area tomorrow, if necessary.
Starting Sunday, the rain chances for East Central Florida are going to be on the increase for the next several days with the rain chances going up to 50%.
I will keep you posted with the recon information if a plane is indeed dispatched to the system.
Read more at the link...
KERRY A. EMANUEL
Center for Meteorology and Physical Oceanography, Massachusetts Institute of Technology, Cambridge, Massachusetts
(Manuscript received 26 December 1995, in final form 18 October 1996)
ABSTRACT
The energy cycle of the mature hurricane resides in the secondary circulation that passes through the storm’s eyewall. By equating the generation of energy in this cycle to boundary layer dissipation, an upper bound on wind speed is derived.
This bound depends on the degree of thermodynamic disequilibrium between the tropical ocean and atmosphere, on the difference between sea surface and outflow absolute temperatures, and also on the ratio between the enthalpy exchange and surface drag coefficients.
Such a bound proves to be an excellent predictor of maximum wind speeds in two different axisymmetric numerical models and does not appear to
depend on the existence of the hurricane eye.
But further consideration of the detailed dynamics of the eye and eyewall show that the intensification of hurricanes is accelerated by feedbacks associated with a component of eye subsidence forced by radial turbulent diffusion of momentum.
This radial momentum diffusion is an inevitable by-product of the strong frontogenesis that the author here shows to be a fundamental characteristic of flow in the eyewall.
Thus, while the upper bound on hurricane wind speed is independent of the eye dynamics, the intensification of hurricanes is indirectly accelerated by turbulent stresses that occur in the eye and eyewall.