| BugsBunny |
| (Weather Watcher) |
| Tue Aug 10 2004 05:52 PM |
|
Re: Here we go...
|
Quote:
The outflow boundaries mentioned earlier for Charley are actually a good thing. these originated from the preceeding band of thunderstorms that may have been inhibiting development of a true CDO.
You seem to be right about Charley; it is becomming more circular in appearance and the shear from earlier is now replaced with good upper-air divergence for the most part, and there is just another 24 hours until it is out of the "graveyard" and I can not really find anything that was not related to a front (such as TD10 in 1994) that has dissipated in the western Caribbean north of 15 degrees.
Charley vis