000 AXPZ20 KNHC 262122 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC WED FEB 26 2014 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. THE FOLLOWING INFORMATION IS BASED ON SATELLITE IMAGERY...WEATHER OBSERVATIONS...RADAR...AND METEOROLOGICAL ANALYSIS. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2100 UTC. ...SPECIAL FEATURE... A STRONG COLD FRONT WILL MOVE INTO THE FORECAST AREA BY THU MORNING EXTENDING FROM 30N137W TO 25N140W WITH WINDS TO GALE FORCE WITHIN 90 NM E OF THE FRONT. THE FRONT WILL RAPIDLY SHIFT EASTWARD WITH MINIMAL GALE FORCE WINDS E OF THE FRONT AND GALE FORCE WINDS TO 40 KT EXPECTED N OF 27N BEHIND THE FRONT THU AND THU NIGHT. SEAS WILL BUILD AS HIGH AS 22 FT IN NW SWELL BY FRI. WINDS WILL DIMINISH BELOW GALE FORCE E OF THE FRONT BY LATE THU NIGHT...BUT WILL CONTINUE TO COVER A PORTION OF THE AREA W OF THE FRONT THROUGH AT LEAST FRI AFTERNOON. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... THE MONSOON TROUGH REMAINS WEAK AND ILL DEFINED ACROSS E PORTIONS OF THE AREA INTO COLOMBIA AND IS BETTER DESCRIBED AS ITCZ. THE ITCZ EXTENDS FROM 06N87W TO 04N95W TO 05N115W. IT THEN RESUMES FROM 05N120W TO BEYOND 06N140W. NO SIGNIFICANT CONVECTION WAS NOTED. ...DISCUSSION... WEAK HIGH PRESSURE OF 1019 MB IS CENTERED OVER THE FORECAST AREA NEAR 25N118W. A DISSIPATING STATIONARY FRONT EXTENDS FROM 30N128W TO 22N140W. AN UPPER LEVEL LOW HAS INDUCED A SURFACE TROUGH FROM 07N117W TO 02N118W. THE PRESSURE GRADIENT BETWEEN THE WEAK HIGH PRESSURE AND THE ITCZ IS ONLY ABLE TO SUPPORT GENTLE TO MODERATE TRADES OVER MUCH OF THE FORECAST AREA. THE SURFACE TROUGH WILL DISSIPATE BY THU. NW SWELLS THAT WERE USHERED IN BY THE FRONTAL BOUNDARY ARE MOVING ACROSS THE NW PART OF THE AREA WITH SEAS IN THE 8 TO 15 FT RANGE FOUND NW OF LINE FROM 30N122W TO 15N140W. THE SWELLS WILL CONTINUE TO PROPAGATE SE OVER THE NEXT COUPLE OF DAYS WITH SEAS 8 FT OR GREATER COVERING MUCH OF THE FORECAST AREA N OF 08N W OF 115W BY FRI AFTERNOON. THE STATIONARY FRONT WILL DISSIPATE BY THU MORNING BEFORE A STRONGER COLD FRONT ENTERS THE AREA...DISCUSSED IN THE SPECIAL FEATURES SECTION. $$ AL