000 AXNT20 KNHC 301728 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 105 PM EST SUN DEC 30 2007 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...THE GULF OF MEXICO...THE CARIBBEAN SEA...NORTHERN SECTIONS OF SOUTH AMERICA...AND THE ATLANTIC OCEAN TO THE AFRICAN COAST FROM THE EQUATOR TO 32N. THE FOLLOWING INFORMATION IS BASED ON SATELLITE IMAGERY...METEOROLOGICAL ANALYSIS... WEATHER OBSERVATIONS...AND RADAR. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1715 UTC ...SPECIAL FEATURE... SURFACE LOW PRES...1008 MB..IS CENTERED OVER THE EASTERN ATLC ABOUT 900 MILES SSW OF THE AZORES. SATELLITE IMAGERY INDICATES THAT THIS SYSTEM IS NOW INTERACTING WITH A COLD FRONT TO ITS N AND SHOWER AND TSTM ACTIVITY HAS BECOME LESS ORGANIZED THAN YESTERDAY. HOWEVER...THIS SYSTEM CONTINUES TO PRODUCE GALE-FORCE WINDS...MAINLY TO THE N AND SLIGHTLY TO THE S OF THE CENTER...AND IT STILL COULD BECOME A SUBTROPICAL STORM LATER TODAY OR TOMORROW AS IT MOVES SLOWLY DURING THE NEXT COUPLE OF DAYS. MOST OF THE CONVECTION IS TO THE N OF THE LOW CENTER FROM 29N-32N BETWEEN 31W-36W...WITH A LINE OF SHOWERS AND POSSIBLE ISOLATED TSTMS FROM 28N34W 28N34W. ...THE ITCZ... FROM 6N11W TO 2N30W TO 1N50W. SCATTERED SHOWERS ARE WITHIN 240 NM N OF THE AXIS W OF 25W. ...DISCUSSION... GULF OF MEXICO... MID/UPPER LEVEL TROUGH IS DIGGING ACROSS TEXAS AND INTO THE FAR NW GULF OF MEXICO. THE GULF OF MEXICO E OF 87W IS COVERED BY ANTICYCLONIC FLOW FROM A RIDGE EXTENDING N FROM THE CARIBBEAN. STATIONARY FRONT EXTENDS FROM NEAR PENSACOLA FLORIDA ACROSS THE MOUTH OF THE MISSISSIPPI TO 25N95W. SCATTERED SHOWERS AND TSTMS ARE ALONG THE FRONT N OF 28N WITH...OVERCAST CLOUDS W OF THE FRONT. CARIBBEAN SEA UPPER LEVEL ANTICYCLONIC CIRCULATION IS CENTERED BETWEEN JAMAICA AND HAITI. MODERATE TO STRONG SUBSIDENCE...WITH DRY AIR AT THE MIDDLE AND UPPER LEVELS OF THE ATMOSPHERE...COVERS NEARLY ALL OF THE CARIBBEAN. HOWEVER..SCATTERED SHOWERS ARE LIKELY IN THE FAST MOVING SCATTERED TO BROKEN LOW CLOUDS E OF 75W AND ALSO ACROSS THE NW CARIBBEAN W OF 85W. ATLANTIC MID/UPPER LEVEL RIDGE ACROSS THE WESTERN ATLC EXTENDS FROM AN ANTICYCLONIC CIRCULATION IN THE CARIBBEAN ACROSS THE SOUTHERN BAHAMAS TO 32N70W. MODERATE TO STRONG SUBSIDENCE COVERS MOST OF THE ATLC S OF 30N W OF 60W. DOWNSTREAM TROUGH WITH AXIS FROM 32N40W TO NEAR WITH WINDWARD ISLANDS 14N59W. AN UPPER LEVEL ANTICYCLONIC CIRCULATION IS E OF THE TROUGH CENTERED NEAR 28N27N WITH RIDGE EXTENDING NWD TO 32N25W. UPPER LEVEL DIFFLUENT FLOW BETWEEN THE TROUGH AND THE RIDGE IS ENHANCING CONVECTIVE ACTIVITY ON THE N SIDE OF LOW PRES DESCRIBED IN SPECIAL FEATURES. A 90-100 KT SUBTROPICAL JETSTREAM EXTENDS FROM 11N51W TO 20N35W THEN TO AFRICA NEAR 25N15W. BROKEN/OVERCAST MIDDLE AND HIGH CLOUDS ARE WITHIN 400 NM S OF THE JET AXIS. TRANSVERSE BANDING IS NOTED ON THE HIGH CLOUDS E OF 35W INDICATING POSSIBLE HIGH LEVEL TURBULENCE. MODERATE/STRONG SUBSIDENCE IS N OF THE JET W OF 40W. $$ DGS