TD Ernesto Satellite,Analysis and Models Thread #8
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- gatorcane
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Actually guys it is very intersting he seems to be drifting a bit E of N....am I seeing something...check it out:
http://radar.weather.gov/radar.php?rid= ... 1&loop=yes
http://radar.weather.gov/radar.php?rid= ... 1&loop=yes
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MBismyPlayground wrote:Anyone, what is baroclinic support ???
In layman's terms -- when you hear baroclinc support, think temperature gradient or front. Baroclinic instability, in contrast to barotropic instability (tropical cyclones are barotropic or equivalent barotropic systems) results from horiztonal temperature gradients. Extratropical cyclones (i.e. mid-latitude lows) derive their "energy" from baroclinicity.
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- MBismyPlayground
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gatorcane wrote:The E drift is significant, if he can manage to go up the east coast just barely offshore - I doubt it would happen but you never know with Ernesto.
Still looking NNW to me judging by this loop. Looks like the COC is right near the "OCR" label.
http://www.sfwmd.gov/org/omd/ops/weather/radamx.html
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CycloneCarl wrote:LeeJet wrote:How the heck do tropical storm winds expand 105 miles from the center when nobody is getting them? Can somebody explain this enigma?
The centre of all tropical cyclones is calm or nearly so. Winds are due to the pressure gradient between the low in the centre and surrounding higher pressures. In a hurricane these usually concentrate in a ring or 'donut' around the centre. In weaker systems the low in the centre is not well defined and strongest winds are usually offset a considerable distance away in the direction of highest pressure.
Yes, but the point is that there are no tropical storm force winds, so how can it expand 105 miles from the center?
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