000 AXPZ20 KNHC 022158 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC SUN APR 02 2006 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 2145 UTC. ...ITCZ... ITCZ AXIS ALONG AXIS 3N78W 5N92W 4N129W 3N140W. SCATTERED MODERATE ISOLATED STRONG WITHIN 90 NM OF AXIS FROM 88W TO 120W AND WITHIN 60 NM OF 6N126W AND 10N128W ASSOCIATED WITH A TROUGH AXIS. ...DISCUSSION... THE NE PAC IS DOMINATED BY A LONGWAVE TROUGH WITH AN EMBEDDED DEEP LAYERED CYCLONE NEAR 45N135W. A SHORTWAVE TROUGH IS SWINGING SE ALONG 34N135W 26N145W ATTM ACCOMPANIED BY A BAND OF DRY UPPER AIR WITHIN 30 NM OF ITS AXIS. ANOTHER SHORTWAVE TROUGH OVER THE CENTRAL CONUS EXTENDS SW INTO THE DISCUSSION AREA FROM 32N103W TO A BASE NEAR 22N109W. AN UPPER CYCLONE HAS CUTOFF AS EXPECTED NEAR 4N118W. SQUEEZED BETWEEN THESE TROUGHS...AN EMBEDDED SHORTWAVE RIDGE ORIGINATES FROM AN ANTICYCLONE NEAR 2N163W...AND EXTENDS NE INTO THE AREA ALONG 17N140W 27N120W TO AN AMPLIFYING CREST OVER NEVADA NEAR 40N117W. A DEEP LAYERED TROUGH HAS DEVELOPED S OF 15N ALONG 130W WITH UPPER DIFFLUENCE NOTED ON LATEST CLOUD MOTION VECTORS. CONVECTION IS FLARING WITHIN 120 NM E OF THE ASSOCIATED LOW LEVEL TROUGH...EXTENDING FROM 3N TO 13N ALONG 130W...AND ALONG THE ITCZ BETWEEN 125W AND 110W. THE RESULTANT DEBRIS MOISTURE IS SPREADING NE TO NEAR 16N115W THEN EVAPORATES. BUT AN INTENSE MOISTURE PLUME THAT BEGINS NEAR THE ANTICYCLONE AT 2N163W LIES ALONG THE SHORTWAVE RIDGE AXIS AND CONTINUES ACROSS NW OLD MEXICO AND SOUTHERN CALIFORNIA INTO THE WESTERN CONUS. A BAND OF DRY AIR IS NOTED WITHIN THE SHORTWAVE TROUGH OVER OLD MEXICO...ROUGHLY TO THE N OF 23N BETWEEN 115W AND 100W...AND IS SHIFTING E WITH TIME. UPPER ANTICYCLONES IS CENTERED OVER N COLOMBIA AND N VENEZUELA WITH A COLLAPSING RIDGE EXTENDING NW ACROSS THE W CARIBBEAN WHERE THE UPPER FLOW HAS BECOME ZONAL. ANOTHER UPPER ANTICYCLONE IS ESTIMATED NEAR 5N92W WITH A RIDGE EXTENDING NNE ACROSS THE W GULF OF MEXICO AND CONTINUING NE ACROSS THE SE CONUS. UPPER DIFFLUENCE UNDER THIS RIDGE IS ENHANCING CONVECTION ALONG THE ITCZ E OF 110W. THE RESULTANT UPPER DEBRIS MOISTURE IS SPREADING NE ACROSS CENTRAL AMERICA AND MERGING INTO THE ZONAL UPPER FLOW DOMINATING MOST OF THE CARIBBEAN. OTHERWISE DRY UPPER AIR DOMINATES THE DISCUSSION N OF THE ITCZ E OF 110W. AT THE SURFACE...HIGH PRES 1023 MB IS QUASI STATIONARY NEAR 28N120W AND IS BLOCKING A WEAKENING FRONTAL TROUGH THAT LIES ALONG 32N125W 21N133W. THE APPROACHING UPPER TROUGH HAS A SURFACE COLD FRONT ALONG 32N132W 28N140W THAT WILL BRING ANOTHER TRAIN OF NW SWELLS INTO THE DISCUSSION AREA. GULF OF PAPAGAYO...LATEST SSMI DATA INDICATE NE WINDS 20 KT WITHIN 60 NM EITHER SIDE LINE 8N94W 11N87W. MODEL GUIDANCE FLUCTUATES NE 20 KT WINDS THROUGH 48 HOURS. $$ NELSON