000 AXPZ20 KNHC 191523 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC SAT DEC 19 2009 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1500 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE...07N78W TO 07N115W TO 07N140W. SCATTERED MODERATE CONVECTION IS WITHIN 60 NM OF 07N81.5W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 60 NM OF THE POINT 07N119W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 90 NM OF THE POINT 07.5N127W. SCATTERED MODERATE CONVECTION IS WITHIN 60 NM OF 09N131W. ...DISCUSSION... STRONG SHORTWAVE IS WEST AND NORTHWEST OF THE AREA AND EXTENDS OVER THE AREA NW OF A LINE THROUGH 32N132W TO 24N140W. ASSOCIATED SURFACE COLD FRONT IS ALONG LINE THROUGH 32N137W TO 28N140W. A PLUME OF UPPER LEVEL MOISTURE WITH BROKEN TO OVERCAST MOSTLY HIGH CLOUDS IS ALSO ASSOCIATED WITH THE TROUGH AND COVERS THE AREA WEST OF 130W. THE MOISTURE EMANATES FROM ITCZ CONVECTION WEST OF THE AREA AND GENERAL RISING MOTION ON THE EAST FLANK OF THE TROUGH WETS OF THE AREA. THE SHORTWAVE JUST NORTHWEST OF THE AREA IS FORECAST TO TRACK EAST REACHING CENTRAL CALIFORNIA LATE SUNDAY. THE LARGER TROUGH IS FORECAST TO REMAIN STATIONARY AND WEAKEN THROUGH THE NEXT COUPLE OF DAYS. ANOTHER TROUGH IS OVER THE NORTH HALF OF MEXICO WITH A TROUGH AXIS ALONG A LINE THROUGH 26N95W TO THE ITCZ NEAR 115W. SOUTHERLY FLOW EAST OF THE TROUGH AXIS IS BRINGING ITCZ MOISTURE NORTH OVER MEXICO EAST OF THE TROUGH AXIS AND ALL OF CENTRAL AMERICA. MULTIPLE LEVEL OVERCAST TO BROKEN CLOUDS ARE NORTH OF THE ITCZ WITH SOME ISOLATED EMBEDDED CONVECTION. STRONG SOUTHWESTERLY WINDS IN THE UPPER LEVELS ARE WITHIN 300 NM SOUTHEAST OF THE TROUGH AXIS. WINDS REACH TO 120 TO 130 KNOTS IN THIS ZONE AND UPPER LEVEL TURBULENCE IS POSSIBLE IN THIS AREA. FROM 115W TO 135W...THE AREA BETWEEN THE TWO TROUGHS...IS A LARGE SCALE DEEP LAYER RIDGE WITH MOSTLY DRY AND CLOUD FREE MIDDLE AND UPPER LEVELS. DIFFLUENT UPPER FLOW OVER THE ITCZ FROM 115W TO 135W IS CAUSING SOME ENHANCEMENT TO THE ITCZ CONVECTION. OTHER THAN THE COLD FRONT MENTIONED ABOVE A WEAK RIDGE IS NORTH OF THE ITCZ WEST OF 108W. ELSEWHERE A BROAD TROUGH CENTERED ON THE ITCZ IS ANALYZED AT THE SURFACE. GAP N TO NE WINDS OF 20 TO 25 KT ARE OCCURRING THROUGH THE GULF OF TEHUANTEPEC AND ARE EXPECTED TO CHANGE LITTLE THROUGH LATE SUN NIGHT. THE COMBINATION OF STRONG TRADE WINDS IN THE CARIBBEAN AND LOCAL DRAINAGE EFFECTS WILL ALLOW FOR NE TO E 20 KT WINDS THROUGH THE GULF OF PAPAGAYO TO PULSATE ON AND OFF WITH MAXIMUM PEAK OCCURRENCES IN THE MORNINGS INTO EARLY NEXT WEEK. FOR ADDITIONAL INFORMATION PLEASE VISIT HTTP://WWW.HURRICANES.GOV/MARINE $$ LL