

The EURO gives a small boost to Caribbean area.
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KWT wrote:Yep Aric its really uncertain what will happen. Current sat.pics certainly would favor a EPAC system but it has to be said in to convergence and voricity argueably would favor the Sw Caribbean, it just needs something to set it off, a spark?
MiamiensisWx wrote:This is not an official forecast or prognosis; it is my personal thoughts on the current situation. Always rely on the TPC and NWS for official data.
Bottom line: "The following post is NOT an official forecast and should not be used as such. It is just the opinion of the poster and may or may not be backed by sound meteorological data. It is NOT endorsed by any professional institution including storm2k.org. For official information please refer to the NHC and NWS products."
Currently, there is a very complex and uncertain battle occurring over the extreme eastern Pacific and southern Caribbean basin, and it will likely be influenced by the evolution of the upper air pattern and low level environment over the next 24 to 48 hours. The most well defined mid-level circulation is evident over extreme eastern Pacific and along western Central America. This is a positive for possible EPAC cyclogenesis. However, it is still entwined with the broad surface trough that extends into the southern Caribbean, and it is still experiencing the resulting effects of upper level westerly shear. Although a surface low is present in the eastern Pacific, there are no signs of a low level circulation in the basin. If the EPAC surface low does not separate from the expansive surface trough over the next 24 to 48 hours, it is very likely that the southern Caribbean will serve as the focal point of cyclogenesis. In fact, there are additional signs that support the Caribbean instead of the EPAC. An upper level ridge will slowly expand over the vicinity during the next 24 to 36 hours, while a very close tropical wave axis and low level convergence line over NW South America will enter the southern Caribbean. The wave axis has remained defined overnight. This will aid lifting mechanisms for convection in the immediate area and support the development of a mesoscale convective system via cyclogenesis. The aforementioned moisture plume will also enter this region. Overall, the region of development (EPAC vs. S Caribbean basin) will likely be decided soon, and the region of the best low level inflow will influence it. I think the EPAC situation is a short lived distraction, while the S Caribbean will eventually win over the next few days. Alberto 2006 is a very decent analog for this system's genesis and early life span.
http://www.ssd.noaa.gov/goes/east/watl/loop-vis.html
The fact that the EPAC surface low is failing to detatch from the surface trough is quickly becoming its worst enemy and the S Caribbean's ally!
gatorcane wrote:Clearly the worst case for the SE US, especially Florida, is that we get a slack moving system over the open waters of the SW and Western Caribbean for a couple of days allowing this low to deepen and then the low eventually finds a weakness in the ridge to the north which would eventually happen....but its way too uncertain at this time what will happen.
actually the GFS keeps sniffing out a weakness to drive whatever is in the Caribbean north and then eventually NE....I think it is picking up on a new system that will approach the Pacific NW and drive SE possibly eroding the ridge over Texas and the northern GOM.