000 AXNT20 KNHC 192341 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 705 PM EST MON JAN 19 2009 TROPICAL WEATHER DISCUSSION FOR NORTH AMERICA...CENTRAL AMERICA...GULF OF MEXICO...CARIBBEAN SEA...NORTHERN SECTIONS OF SOUTH AMERICA...AND 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 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2315 UTC. ...THE ITCZ... THE ITCZ AXIS IS CENTERED ALONG 6N10W 2N20W 1N30W CROSSING THE EQUATOR NEAR 37W AND EXTENDING INTO NE BRAZIL NEAR 3S45W. SCATTERED MODERATE/ISOLATED STRONG CONVECTION IS WITHIN AROUND 100 NM SOUTH OF AXIS BETWEEN 15W-31W. CLUSTERS OF MODERATE TO STRONG CONVECTION ARE NOTED ALONG THE NORTHERN COAST OF BRAZIL AND OVER FRENCH GUIANA AND SURINAME. ...DISCUSSION... GULF OF MEXICO... A DEEP-LAYERED TROUGH OVER THE E CONUS AND THE NORTHERN GULF WATERS SUPPORTS A COUPLE OF COLD FRONTS CURRENTLY LOCATED OVER THE GULF REGION. STRONG WESTERLY FLOW ALOFT WITH CORE WINDS OF 110-130 KT IS OBSERVED IN THE BASE OF THIS TROUGH AFFECTING MUCH OF THE GULF AND THE FLORIDA PENINSULA. AT 19/2100 UTC...ONE COLD FRONT EXTENDS FROM SW FLORIDA TO THE YUCATAN PENINSULA AND WILL MOVE SE OF THE AREA EARLY TONIGHT. A SECOND FAST MOVING COLD FRONT STRETCHES FROM THE WESTERN FLORIDA PANHANDLE TO BROWNSVILLE TEXAS. THIS FRONT IS FORECAST TO MOVE ACROSS SOUTH FLORIDA AND THE SE PORTION OF THE GULF TUE MORNING CLEARING THE AREA BY EARLY TUESDAY AFTERNOON. IN THE WAKE OF THE FRONT... BRISK NLY WINDS AND VERY STRONG COLD AIR ADVECTION ARE EXPECTED WITH THE RISK OF A SNOW FLAKE OR TWO AS SOUTH AS THE AREA OF TAMPA. THIS IS PROBABLY SO FAR THE COLDEST AIR OF THE SEASON. HIGH PRES WILL BUILD IN BEHIND THE SECOND FRONT. CARIBBEAN SEA... UNDER THE INFLUENCE OF A BROAD MID/UPPER-LEVEL RIDGE...DRY AIR AND STABLE ATMOSPHERIC CONDITIONS ARE AFFECTING MUCH OF THE CARIBBEAN SEA. AS A RESULT...GENERALLY FAIR WEATHER PREVAILS ACROSS THE MAJORITY OF THE AREA. HOWEVER...A SURFACE TROUGH EXTENDING FROM JAMAICA TO EASTERN PANAMA IS GENERATING A NARROW BAND OF MAINLY LOW/MID CLOUDS AND SCATTERED SHOWERS OVER THE CENTRAL CARIBBEAN. VIS SATELLITE IMAGERY REVEALS A SWIRL OF LOW CLOUDS ALONG THE TROUGH AXIS NEAR 12.5N. THIS TROUGH WILL CONTINUE TO DRIFT W AND DISSIPATE ALONG 80W TONIGHT. PATCHES OF LOW LEVEL MOISTURE ARE OVER HISPANIOLA AND THE WINDWARD PASSAGE AS WELL AS OVER PARTS OF HONDURAS AND GUATEMALA. THE NEXT COLD FRONT WILL MOVE THROUGH THE YUCATAN CHANNEL LATE TUE REACHING FROM HISPANIOLA TO NICARAGUA LATE WED. NW WINDS OF 20 KT WILL FOLLOW THE FRONT. MODERATE TRADE WINDS ARE BLOWING ACROSS THE BASIN. ATLANTIC OCEAN... A JET-STREAM BRANCH WITH CORE WINDS OF 130-150 KT IS OVER CENTRAL FLORIDA AND THE W ATLC AHEAD OF A DEEP-LAYERED TROUGH LOCATED OVER THE EASTERN CONUS. THE STRONG WESTERLY WINDS ALOFT ARE REACHING CUBA AND THE NW CARIBBEAN N OF 20N. THE DEEP TROUGH IS ASSOCIATED WITH A SURFACE COLD FRONT THAT ENTERS THE FORECAST 31N75W THEN CONTINUES SW ACROSS SOUTH FLORIDA AND THE GULF OF MEXICO. SW WINDS WITH GALE FORCE ARE BLOWING WITHIN 240 NM E OF THE FRONT AND N OF OF 27N. LOW LEVEL CONVERGENCE IS SUPPORTING SCATTERED SHOWERS AND ISOLATED TSTMS WITHIN 60 NM EITHER SIDE OF THIS COLD FRONT. ADDITIONALLY...A SECOND COLD FRONT IS FORECAST TO MOVE OFF THE SE UNITED STATES COAST LATE TONIGHT...REACHING A LINE FROM 31N70W TO THE FLORIDA STRAITS TUESDAY MORNING. FURTHER EAST...A STATIONARY FRONT ENTERS THE AREA NEAR 31N60W THEN CONTINUES SW TO NEAR 27N65W. AT THIS POINT...IT BECOMES A SURFACE TROUGH AND EXTENDS SW TO NEAR THE TURKS AND CAICOS ISLANDS. SCATTERED SHOWERS ARE ALONG THE FRONT/TROUGH AXIS. A SFC RIDGE ANCHORED BY A 1033 MB HIGH LOCATED NEAR 32N37W DOMINATES MOST OF THE EAST AND CENTRAL ATLC RESULTING IN MOSTLY FAIR WEATHER AND MODERATE TO STRONG TRADE WINDS. THIS HIGH PRES CENTER WILL DISSIPATE IN ABOUT 24 HOURS BUT A STRONGER ONE... ANALYZED 1038 MB TO THE NORTH...WILL REMAIN IN PLACE COVERING THE REGION. ACROSS THE TROPICAL ATLC...WESTERLY FLOW ALOFT IS PRESENT...WITH UPPER LEVEL DIVERGENCE ENHANCING THE CONVECTION ASSOCIATED WITH THE ITCZ. $$ GR