000 AXNT20 KNHC 292348 TWDAT TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 705 PM EST TUE JAN 29 2008 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 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2245 UTC ...THE ITCZ... ITCZ AXIS IS CENTERED ALONG 5N8W 6N12W 3N29W 5N41W 3N52W. CLUSTERS OF SCATTERED MODERATE/ISOLATED STRONG CONVECTION ARE WITHIN 75 NM OF THE ITCZ AXIS FROM 23W-35W. ...DISCUSSION... GULF OF MEXICO... HIGH PRESSURE IS RETREATING EASTWARD PRECEDING THE APPROACHING COLD FRONT THAT IS CURRENTLY INLAND OVER CENTRAL TEXAS. A SURFACE TROUGH IS ALONG THE THE TEXAS COAST INDICATED BY A WIND SHIFT. THE ASSOCIATED DEEP LAYERED TROUGH IS OVER THE CENTRAL PLAIN STATES JUST W OF THE MISSISSIPPI VALLEY. THIS FRONT WILL ENTER THE GULF DURING THE NIGHT TONIGHT. SCATTERED SHOWERS/ ISOLATED THUNDERSTORMS ARE OVER THE NW GULF WITHIN 30 NM OF LINE FROM 28N95W TO INLAND OVER LOUISIANA NEAR VERMILION BAY. BROAD UPPER RIDGE COVERS THE GULF WITH THE AXIS EXTENDING FROM S MEXICO AND THE E BAY OF CAMPECHE TO OVER NE FLORIDA AND ALONG THE CAROLINA COASTS. SOUTHERLY SURFACE FLOW DOMINATES THE GULF DUE TO THE APPROACHING FRONT AND THE RETREATING SURFACE HIGH. DRY STABLE AIR REMAINS OVER THE S GULF AND S FLORIDA PENINSULA. CARIBBEAN SEA... BROAD DEEP LAYERED TROUGH IN THE W ATLC EXTENDS S INTO THE CARIBBEAN N OF 16N W OF 71W ACROSS THE LEEWARD ISLANDS WITH THE ASSOCIATED COLD FRONT DISSIPATING ACROSS THE VIRGIN ISLANDS/ PUERTO RICO TO NEAR 15N73W. ISOLATED SHOWERS ARE WITHIN 90 NM E OF THE FRONTAL BOUNDARY. BASED ON WATER VAPOR IMAGERY THE CARIBBEAN IS UNDER SOME VERY DRY STABLE AIR AT THE UPPER LEVELS. HOWEVER THERE IS ENOUGH LOW LEVEL MOISTURE TO GENERATE SCATTERED LOW CLOUDS WITH POSSIBLE ISOLATED SHOWERS MAINLY OVER THE E CARIBBEAN. A SURFACE TROUGH IS JUST E OF THE LESSER ANTILLES GENERATING SOME ISOLATED SHOWERS OVER THE REMAINDER OF THE ISLANDS. DENSE LOW CLOUDS WITH SCATTERED SHOWERS ARE OVER NICARAGUA DUE TO THE EASTERLY TRADE WINDS AND THE REMNANTS OF THE ABOVE FRONT. ATLANTIC OCEAN... THE UPPER RIDGE THAT COVERS THE GULF OF MEXICO EXTENDS OVER THE W ATLC W OF 72W. A DEEP LAYERED TROUGH COVERS THE REMAINDER OF THE W ATLC INTO THE CENTRAL ATLC AND N CARIBBEAN FROM 55W-72W WITH THE ASSOCIATED COLD FRONT ENTERING THE REGION NEAR 32N53W EXTENDING SSW ALONG 25N58W TO THE VIRGIN ISLANDS/PUERTO RICO NEAR 18N65W THEN DISSIPATING INTO THE CARIBBEAN. SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS ARE WITHIN 90/120 NM E OF THE FRONT WITH COLD AIR STRATOCUMULUS CLOUDS COVERING THE AREA W OF THE FRONT TO 75W. A WEAKENING SURFACE TROUGH IS JUST TO THE E OF THE FRONT EXTENDING FROM 23N56W TO JUST E OF THE LESSER ANTILLES NEAR 15N62W GENERATING SOME SCATTERED SHOWERS WITHIN 75 NM E OF THE TROUGH AND ISOLATED SHOWERS OVER THE CARIBBEAN ISLANDS. NARROWING UPPER LEVEL RIDGE COVERS THE REMAINDER OF THE CENTRAL ATLC ANCHORED DEEP IN THE TROPICS WITH THE MEAN AXIS ALONG 47W. BROAD UPPER TROUGH COVERS THE E ATLC N OF 17N E OF 40W WITH THE AXIS EXTENDING THROUGH 32N22W TO AN UPPER LOW NEAR 27N27W TO 17N32W. SCATTERED SHOWERS AND POSSIBLE ISOLATED THUNDERSTORMS ARE WITHIN 200 NM OF THE UPPER LOW. THE REMNANTS OF A STATIONARY BOUNDARY JUST DIP INTO THE REGION THROUGH 32N29W TO 28N35W. $$ WALLACE