Atmosphere is primed
Posted by JAC on 6/10/2009, 7:52 am

Shear is a combination of upper and lower winds.
When a TC forms, the lower winds circulate in a CCW direction; no longer in a unified single direction.
So, the lower wind component of the shear goes away. 
UL winds are key to watch. 
15 knots is not too bad.
A good hot-tower can redirect that and possibly form an anti-cyclone.
If an anti-cyclone forms, then the upper-component of shear goes away as well.

Currently in the West Carib:
MSLP at 29.87"
Ozone shows a high tropopause.

Ready for a warm-core to form.

Actually, GOM ozone is abnormally low as well.







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GFS & CMC Back on for West Carib Development - JAC, 6/10/2009, 5:56 am
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