#10 Postby Hyperstorm » Mon Dec 27, 2004 8:43 pm
Based on some quick satellite observations, the system appears to have an even tigher core than yesterday and it appears to have acquired a few tropical characteristics (tighter core/slowly detaching from troughiness/moderate convection on east side). Of course, this contrasts with the extratropical characteristics it mostly possesses (large windfield/still attached with trough/cold core). The longer it sits over those relatively warmer waters (causing convection to build up) the closer it will be to transition.
The main inhibiting factor for this cold core low to quickly transition is climatology, which means a strong jet of shear just about everywhere in the Atlantic. Just to find perfect conditions will be a virtually impossible task, however, there is not enough shear to completely destroy it as of now. If it can maintain that southern latitude, it could remain over slightly more favorable waters and have additional development. I'll watch out for that.
Nothing to get excited about just yet, but we could have a system that can rival 1955's Alicia in being a cyclone in 2 different years. Of course, if this indeed exhibits characteristics, it will all come down to NHC pressing the green button.
I can't believe it's been a month since we had the same kind of setup...
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