THE MAIN WEATHER FEATURE ACROSS THE FORECAST AREA IS A 1005 MB
LOW SPINNING NEAR 28N37W. THIS LOW REMAINS QUASI-STATIONARY. THE
AIR MASS AROUND THIS LOW HAS BECOME MORE HOMOGENEOUS DURING THE
LAST 24 HOURS...AND THERE ARE NO FRONTS ASSOCIATED WITH THIS
CYCLONE ANY LONGER. INSTEAD...A SFC TROUGH IS ANALYZED FROM THE
SFC LOW TO 20N41W. SCATTERED SHOWERS AND TSTMS ARE MOST
ORGANIZED IN BANDS N AND NE OF THE LOW. TIGHT PRES GRADIENT
BETWEEN THIS CYCLONE AND HIGH PRES OVER THE CENTRAL ATLC IS
PRODUCING A LARGE AREA OF MODERATE TO STRONG NE WINDS IN THE NW
SEMICIRCLE OF THE LOW. ACCORDING TO THE GFS COMPUTER MODEL...THE
LOW WILL SLOWLY DRIFT SW AND WEAKEN DURING THIS WEEKEND. MOST OF
THE WEST AND CENTRAL ATLC ARE UNDER THE INFLUENCE OF A RIDGE
ANCHORED ON A 1031 MB HIGH LOCATED NEAR 36N52W. FRAGMENTS OF LOW
LEVEL CLOUDS ARE OBSERVED ACROSS THE AREA WITH SLY RETURN FLOW
ACROSS THE BAHAMAS AND THE WESTERN ATLC WEST 0F 70W. ALOFT...A
RIDGE/TROUGH/RIDGE PATTERN DOMINATES THE AREA. A JET STREAM
BRANCH WITH CORE WINDS OF 90-130 KT LIES BETWEEN THE PREVIOUSLY
MENTIONED LARGE CUT-OFF LOW OVER THE EASTERN ATLC AND A BROAD
UPPER-LEVEL HIGH LOCATED SE OF THE CAPE VERDE ISLANDS NEAR
9N18W. UPPER SLY FLOW ON THE WESTERN SIDE OF THE HIGH IS
ADVECTING PATCHY HIGH LEVEL CLOUDS FROM N SOUTH AMERICA ACROSS
THE TROPICAL ATLC. THESE WINDS ARE ALSO ENHANCING SCATTERED
MODERATE CONVECTION N OF THE ITCZ AXIS AND WEST OF 40W.
http://www.nhc.noaa.gov/text/refresh/MIATWDAT+shtml/071752.shtml?No one posted the TWD.
Personally, I think it has a chance, though it will not threaten any land masses.