When I thought the shear was supposed to remain low, I kind of thought it might survive without convection and might possibly make it past the dry air and shear, but things are looking rather hostile ahead:
http://www.ssd.noaa.gov/goes/east/carb/loop-wv.htmlIt needs to stay very, very low to have anything more than an outside chance, unless something changes.
If anything survives and passes into the west Carib, which is very hard to make out on most models, then it might have a chance. I have looked for any sign of a remnant surviving and have trouble finding anything that makes it to the west Carib, assuming that is where it might be headed.
Right now it is holding its own despite the dry air:
http://www.ssd.noaa.gov/goes/flt/t1/wv-l.jpgI thought the convection would have left it a few days ago and we might be tracking a LLC on visible sat that made it to the Carib where there would be less shear, if it were to survive. But then it became clearer that shear would increase.
It just doesn't seem like this setup of dry air and shear will change by the time this area makes it to the Islands. But if it were to stay as low as Barbados like you think it might, then perhaps, but I have no clue.
There's a lot going against it right now. With more dry air around it now than yesterday, it seems more likely that the convection it developed in the overnight will diminish more quickly, but that is just a guess.
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From the 5:30AM EDT NHC Atlantic Tropical Weather Outlook:
"A WELL-DEFINED LOW PRESSURE AREA OVER THE CENTRAL ATLANTIC OCEAN IS
LOCATED ABOUT 1000 MILES EAST OF THE SOUTHERN WINDWARD ISLANDS
MOVING WESTWARD AT 10 TO 15 MPH. THIS SYSTEM HAS SOME POTENTIAL FOR
TROPICAL CYCLONE FORMATION DURING THE NEXT DAY OR SO BEFORE
UPPER-LEVEL WINDS BECOME LESS FAVORABLE FOR DEVELOPMENT."