000 AXPZ20 KNHC 052213 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC TUE FEB 05 2008 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2130Z UTC. ...ITCZ... ITCZ AXIS IS ALONG LINE FROM 3N78W 5N100W 8N124W 4N140W 5N140W. SCATTERED MODERATE CONVECTION WITHIN 120 NM OF EITHER SIDE OF LINE ALONG 12N FROM 111W TO 125W. ...DISCUSSION... W OF 105W...BROAD MID/UPPER LEVEL TROUGH EXTENDING FROM SOUTHERN ROCKIES THROUGH NORTHERN MEXICO TO AROUND 19N113W LIFTS OUT AHEAD OF RIDGE ALONG ROUGHLY 140W BUILDING E. A 1034 MB SURFACE HIGH ASSOCIATED WITH THE UPPER RIDGE IS CENTERED NEAR 35N140W. DIVERGENCE ALOFT TO THE SE OF THE UPPER TROUGH CONTINUES TO SUPPORT A SURFACE TROUGH NEAR 123W ALONG THE ITCZ...WITH ASSOCIATED CONVECTION AS DESCRIBED ABOVE. FRESH TO STRONG TRADES REMAIN ACTIVE BETWEEN THIS FEATURE AND THE SURFACE HIGH TO THE NW. IN ADDITION...SCATTEROMETER DATA SHOW NW WINDS TO AROUND 20 KT THROUGH THE GULF OF CALIFORNIA ON THE ERN PERIPHERY OF THE SURFACE HIGH PRESSURE. A WEAK UPPER TROUGH IS DIGGING EWD OVER THE N PACIFIC...FLATTENING OUT THE MID/UPPER RIDGE. THIS WILL LIFT OUT TONIGHT...LEAVING THE RIDGE TO BUILD E THROUGH THE NEXT 48 HOURS. THIS WILL REINFORCE THE ASSOCIATED SURFACE HIGH AS SHIFTS EWD THROUGH THU...KEEPING TRADE WIND FLOW TO THE SOUTH ACTIVE. THE SURFACE HIGH WILL WEAKEN FRI INTO THE WEEKEND AS A MID/UPPER TROUGH DIGS EWD THROUGH THE N PACIFIC AND WEAKENS THE RIDGE. MEANWHILE LARGE NWLY SWELL OF UP TO 12 FT WITH PERIODS TO 13 SECONDS CONTINUE TO PUSH INTO THE AREA FROM THE N CENTRAL PACIFIC. E OF 105W...HIGH RESOLUTION SCATTEROMETER DATA SHOW WINDS THROUGH THE GULF OF PAPAGAYO FINALLY DIMINISHED BELOW 20 KT. SURFACE HIGH PRES BUILDING BEHIND A COLD FRONT MOVING THROUGH THE GULF OF MEXICO WILL INDUCE FRESH NLY FLOW THROUGH THE GULF OF TEHUANTEPEC BY LATE WED. HOWEVER...THIS WILL BE SHORT LIVED...AS THE SURFACE RIDGE TO THE N SHIFTS RAPIDLY E...ALLOWING RETURN FLOW OVER THE WESTERN GULF OF MEXICO AND SHUTTING DOWN THE GAP WINDS THROUGH THE TEHUANTEPEC ISTHMUS. ALOFT UPPER RIDGE DOMINATES. AREA REMAINS VOID OF CONVECTION AS DEEP LAYER MOISTURE REMAINS LACKING. $$ CHRISTENSEN