000 AXPZ20 KNHC 222203 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC TUE DEC 22 2009 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 2130 UTC. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 7N80W 5N90W 4N103W 5N115W 8N122W 8N131W 9N140W. SCATTERED MODERATE CONVECTION IS WITHIN 120 NM S OF THE AXIS E OF 79W. ...DISCUSSION... LONGWAVE TROUGH W OF THE AREA APPROACHING 144W WILL CONTINUE EASTWARD EXPECTED TO MOVE INTO THE WESTERN PORTION OF THE AREA WITHIN THE NEXT 24 HRS. A SMALL CYCLONIC CIRCULATION E OF THE TROUGH HAS PULLED NNE IS PRESENTLY JUST NW OF THE AREA NEAR 31N138W. E OF THE AREA OVER THE DISCUSSION AREA...BROAD MID/UPPER ANTICYCLONIC FLOW IS RATHER PRONOUNCED WITH A MEAN RIDGE AXIS EXTENDING FROM 30N128W TO 20N124W TO 15N122W TO NEAR 8N118W. A JET STREAM BRANCH ENTERS THE AREA AHEAD OF THE TROUGH THROUGH 22N140W...AND EXTENDS NE 29N131W THEN CONTINUES E TOWARDS CENTRAL BAJA CALIFORNIA. STRONG SW TO W WINDS WITH SPEEDS OF 60-90 KT ARE WITHIN THE JET CORE FROM 23N TO 27N BETWEEN 120W AND 131W. OVER THE FAR NE PORTION...A STRONG SHORTWAVE TROUGH HAS JUST ABOUT MOVED INLAND SOUTHERN CALIFORNIA WITH FAST WLY FLOW FOLLOWING BEHIND IT. THE ASSOCIATED SURFACE COLD FRONT EXTENDS FROM FAR NW MEXICO SW TO CENTRAL BAJA CALIFORNIA NEAR 28N114W AND TO NEAR 26N117W WHERE IT BECOMES RATHER DIFFUSE. A PLUME OF UPPER LEVEL MOISTURE CONSISTING OF BROKEN TO OVERCAST MID AND HIGH CLOUDS DUE TO THE TROUGH COVERS THE EASTERN SECTION OF THE AREA WITHIN 150 NM EITHER SIDE OF A LINE FROM 24N123W TO 25N117W TO ACROSS CENTRAL BAJA AND TO ACROSS NORTHERN MEXICO. THE MOISTURE EMANATES FROM ITCZ CONVECTION WEST OF 130W AND ALSO DUE TO THE GENERAL RISING MOTION ON THE EAST FLANK OF THE TROUGH. MOISTURE AND MULTIPLE LEVEL BROKEN TO OVERCAST CLOUDS ARE OVER MEXICO NORTH OF 24N AND ARE ASSOCIATED WITH THE SHORTWAVE APPROACHING FROM THE WEST. ANOTHER TROUGH IS OVER EASTERN MEXICO WITH A NEGATIVELY TILTED TROUGH AXIS FROM THE YUCATAN PENINSULA NEAR 21N88W TO SOUTHWESTERN COLOMBIA. SOUTHERLY FLOW EAST OF THE TROUGH AXIS IS BRINGING MOISTURE FROM ITCZ CONVECTION NORTH OVER CENTRAL AMERICA EAST OF COSTA RICA. DRYING IS NOTED OVER COSTA RICA WESTWARD AS THE TROUGH SWINGS EAST. IN THIS MOIST REGION MULTIPLE LEVEL OVERCAST TO BROKEN CLOUDS ARE NORTH OF THE ITCZ WITH SOME EMBEDDED CONVECTION. WEST OF THE TROUGH AXIS AND EAST OF THE MOISTURE MENTIONED IN THE FIRST PARAGRAPH...THAT IS THE AREA BETWEEN THE TWO TROUGHS ...IS A LARGE SCALE DEEP LAYER WEAKENING RIDGE WITH MOSTLY DRY AND CLOUD FREE MIDDLE AND UPPER LEVELS. OTHER THAN THE COLD FRONT MENTIONED ABOVE A WEAK RIDGE IS NORTH OF 15N. WEAK LOW PRESSURE 1011 MB IS CENTERED NEAR 14N124W WITH A BROAD TROUGH SOUTH TO THE ITCZ. OTHERWISE A BROAD TROUGH CENTERED ON THE ITCZ IS ANALYZED AT THE SURFACE. GAP N WINDS OF 20 KT ARE OCCURRING THROUGH THE GULF OF TEHUANTEPEC AND ARE EXPECTED TO DIMINISH WITHIN ABOUT 6 HRS. FOR ADDITIONAL INFORMATION PLEASE VISIT HTTP://WWW.HURRICANES.GOV/MARINE $$ AGUIRRE