000 AXPZ20 KNHC 170301 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC WED MAR 17 2010 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0100 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE WAS ANALYZED FROM 04N77W TO 03N90W TO 04N105W TO 04N115W TO 04N140W. SCATTERED MODERATE CONVECTION WAS WITHIN 270 NM N OF THE ITCZ AXIS BETWEEN 82W AND 90W AS WELL AS WITHIN 210 NM N OF THE ITCZ AXIS E OF 78W AND S OF THE ITCZ AXIS TO EQUATOR E OF 81W. A TROUGH IS EMBEDDED IN THE ITCZ FROM 09N103W TO 01N109W. ISOLATED MODERATE CONVECTION WAS WITHIN 210 NM E OF THE TROUGH. ...DISCUSSION... A BROAD UPPER LEVEL TROUGH IS OVER THE FAR NW PORTION OF THE DISCUSSION AREA N OF 25N W OF 125W. A 100-120 KT JETSTREAM IS ROUNDING THE SOUTH SIDE OF THE TROUGH AND IS CENTERED ALONG 27N W OF 125W. DOWNSTREAM UPPER LEVEL RIDGE COVERS THE AREA N OF 20N E OF 120W. STRONG SUBSIDENCE WITH DRY STABLE AIR AT THE MIDDLE AND UPPER LEVELS OF THE ATMOSPHERE IS WITHIN THE RIDGE. ANOTHER UPPER LEVEL TROUGH EXTENDS FROM A WELL DEFINED CYCLONIC CIRCULATION OVER EASTERN TEXAS ACROSS THE WESTERN GULF OF MEXICO TO JUST W OF THE ISTHMUS OF TEHUANTEPEC. SW FLOW SE AND S OF THE TROUGH IS ADVECTING ABUNDANT TROPICAL MOISTURE ALOFT ACROSS SOUTHERN MEXICO. IN THE DEEP TROPICS...AN ANTICYCLONIC CIRCULATION IS CENTERED NEAR 07N91W WITH A RIDGE EXTENDING FROM THE ANTICYCLONE W TO 07N115W AND E INTO SOUTHERN COSTA RICA/NW PANAMA. MODERATE TO STRONG SUBSIDENCE IS FOUND OVER CENTRAL AMERICA NORTH OF THE RIDGE AXIS. SCATTERED MODERATE TO STRONG CONVECTION WAS NEAR THE ITCZ E OF 81W UNDER WEAKLY DIFFLUENT FLOW ALOFT NEAR THE COAST OF COLOMBIA/ECUADOR. STATIONARY FRONT EXTENDS FROM 30N131W TO 26N140W. NE WINDS OF 20-25 KT WERE W OF THE FRONT WITH SEAS 14 TO 17 FT IN NW SWELL. THE FRONT IS FORECAST TO DISSIPATE OVERNIGHT. THE ASCAT PASS FROM 1810 UTC SHOWS FRESH TRADES ARE CONFINED PRIMARILY FROM 07N TO 18N W OF 125W. A TROUGH IS ANALYZED EMBEDDED IN THE ITCZ FROM 09N103W TO 01N109W. CONVECTION HAS WANED OVER THE PAST FEW HOURS NEAR THIS FRONT AS THE DIFFLUENT REAR RIGHT QUADRANT OF THE UPPER JET THAT EXTENDS FROM THE GULF OF MEXICO TO NEAR 11N106W HAS PULLED EASTWARD AND WEAKENED. GAP WINDS IN THE GULF OF TEHUANTEPEC ARE BELIEVED TO HAVE INCREASED ABOVE 20 KT. THE HIGH RESOLUTION ASCAT PASS FROM 1628 UTC SHOWED N WINDS TO 20 KT NEAR THE COAST WHILE THE VISIBLE SATELLITE IMAGERY FROM 1715 TO 1945 UTC SHOWED A ROPE CLOUD TYPICALLY FOUND ON THE LEADING EDGE OF THE WIND SURGE PASSING S AWAY FROM THE GULF OF TEHUANTEPEC. WINDS WILL BLAST QUICKLY TO GALE FORCE OVERNIGHT AS STRONG HIGH PRES BUILDS OVER THE WESTERN GULF OF MEXICO AND TIGHTENS THE PRESSURE GRADIENT OVER SOUTHERN MEXICO. GALES ARE EXPECTED TO PERSIST THROUGH 48 HOURS BEFORE DIMINISHING...WITH WINDS REACHING NEAR STORM FORCE ON WED. FOR ADDITIONAL INFORMATION PLEASE VISIT HTTP://WWW.HURRICANES.GOV/MARINE $$ SCHAUER