000 AXPZ20 KNHC 011512 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC TUE JAN 01 2008 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0800 UTC. ...ITCZ... INTERTROPICAL CONVERGENCE ZONE AXIS RUNS ALONG THE LINE...6N77W 8N110W 8N115W 8N140W. SCATTERED MODERATE ISOLATED STRONG CONVECTION IS WITHIN 170 NM N OF AXIS BETWEEN 111W AND 118W. SIMILAR CONVECTION IS NOTED NEAR 8N135W. ...DISCUSSION... A CUT-OFF LOW LOCATED NEAR 27N121W IS MOVING NE ACROSS THE FORECAST AREA WITH AN UPPER-LEVEL TROUGH EXTENDING SOUTH ALONG 120W TO NEAR 18N. DRY UPPER AIR IS NOTED BEHIND THE TROUGH AXIS FROM 20N TO 25N BETWEEN 120W AND 130W WHILE AMPLE UPPER LEVEL MOISTURE IS SEEN ON THE EAST SIDE OF THE TROUGH AXIS SPREADING OVER THE BAJA PENINSULA/NW MEXICO AND THE STATES OF CALIFORNIA AND ARIZONA. AN UPPER-LEVEL RIDGE ANCHORED ON A HIGH JUST N OF HISPANIOLA DOMINATES SOUTH MEXICO AND THE EPAC E OF 110W. THIS FEATURE IS ENHANCING CONVECTION ALONG THE ITCZ. A DEEP LAYERED TROUGH IS DIGGING INTO THE AREA FROM THE NW SUPPORTING A STRONG COLD FRONT THAT WILL APPROACH THE REGION FROM THE NW IN THE NEXT COUPLE OF DAYS...PRECEDED BY LARGE NW SWELL. HIGH PRES DOMINATES THE AREA N OF THE ITCZ W OF 110W WITH THE EASTERLY TRADES S OF THE RIDGE IN THE 20-25 KT RANGE. THESE WINDS ARE EXPECTED TO DIMINISH TO ABOUT 20 KT AS THE RIDGE WEAKENS AND SHIFTS EASTWARD IN ADVANCE OF THE AFOREMENTIONED COLD FRONT. SOUTH OF THE ITCZ...THE AREA IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS WITH LARGE AREAS OF BROKEN TO OVERCAST STRATOCUMULUS CLOUDS IN THE LOWER ATMOSPHERE. A STRONG REINFORCING SHOT OF COLD AIR IS ENTERING THE NW GULF OF MEXICO THIS MORNING...AND WILL BRING STORM CONDITIONS TO THE GULF OF TEHUANTEPEC AREA BY WED MORNING. STRONG ELY WINDS OVER THE CARIBBEAN WILL BRING NEAR GALE CONDITIONS TO THE GULF OF PAPAGAYO BY TOMORROW MORNING. LARGE ELY SWELL WILL EMERGE FROM BOTH AREAS EARLY THU OVER PORTIONS OF THE E PACIFIC. MEANWHILE NW WINDS OVER THE GULF OF CALIFORNIA ARE THE RESULT OF FUNNELING ON THE PERIPHERY OF SURFACE HIGH PRES FURTHER W. THIS WILL PERSIST THROUGH 24 HOURS THEN DIMINISH AS STRONGER HIGH PRES BUILDS OVER THE GULF OF MEXICO. $$ GR