000 AXPZ20 KNHC 280318 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC MON APR 28 2008 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0300 UTC. ...ITCZ... ITCZ AXIS ALONG 03N78W TO 05N90W TO 06N120W TO 04N128W TO 02N140W. SCATTERED MODERATE AND EMBEDDED ISOLATED STRONG CONVECTION IS WITHIN 90 NM EITHER SIDE OF THE AXIS BETWEEN 102W-107W. WIDELY SCATTERED MODERATE CONVECTION IS WITHIN 120 NM EITHER SIDE OF AXIS BETWEEN 88W-98W. ISOLATED MODERATE CONVECTION IS WITHIN 150 NM N OF AXIS BETWEEN 108W-128W. ...DISCUSSION... W OF 100W... AN AMPLIFIED MID-UPPER PATTERN REMAINS OVER THE REGION WITH A SPRAWLING RIDGE BEING THE MAIN FEATURE ROUGHLY ALONG 123W. DIFFLUENCE ALOFT TO THE W OF THE RIDGE AXIS...ASSOCIATED WITH A SERIES OF SHORTWAVES N AND W OF THE REGION...IS PRODUCING ABUNDANT CLOUDINESS AND SCATTERED SHOWERS S OF 16N W OF 126W AND SCATTERED TO BROKEN MID-HIGH LEVEL CLOUDS FROM 20N-25N W OF 135W. THIS BLOCKING RIDGE IS PREVENTING A FRONT ALONG THE NW CORNER OF THE DISCUSSION ZONE...30N140W...TO MAKE MUCH FURTHER PROGRESS INTO THE REGION. UPPER CONFLUENCE TO THE E OF THE RIDGE AXIS...GREATLY ENHANCED BY A LARGE SCALE TROUGH EXTENDING SSW FROM CENTRAL CANADA TO THE SOUTHERN TIP OF BAJA...IS PRODUCING A VERY DRY ATMOSPHERE FROM 17N-29N E OF 126W. A SUBTROPICAL JET ORIGINATES JUST SE OF THE TROUGH BASE AND IS GENERATING AND TRANSPORTING A PLUME OF HIGH LEVEL MOISTURE WITHIN 300 NM SE OF A LINE FROM 16N110W TO INLAND OVER MAINLAND MEXICO NEAR 25N100W. THIS TROUGH AND ASSOCIATED JET IS PRODUCING SIGNIFICANT TSTM ACTIVITY OVER PORTIONS OF MEXICO AND THE GULF OF MEXICO. IN THE LOWER LEVELS...BESIDES FOR THE AFOREMENTIONED WEAKENING STATIONARY FRONT...A 1029 MB SUBTROPICAL HIGH IS IN CONTROL PRODUCING AN AREA OF N WINDS NEAR 20 KT N OF 27N BETWEEN 121W-127W AND SIMILAR MAGNITUDE NE TRADES OVER THE SW PORTION OF THE ZONE. N TO NE WINDS NEAR 20 KT WILL EXPAND AND COVER MUCH OF THE REGION BY TUE AS HIGH PRES SHIFTS E AND STRENGTHENS. E OF 100W... LIGHT SLY FLOW ALOFT LIES OVER MUCH OF THIS TROPICAL PORTION ON THE W SIDE OF UPPER RIDGING EXTENDING FROM COLOMBIA TO THE YUCATAN CHANNEL. THIS FLOW IS DRAWING ITCZ-MOISTURE NWD TOWARD THE COAST OF CENTRAL AMERICA...THOUGH MOST OF DEEP MOISTURE IS FARTHER W OVER MEXICO TRIGGERED BY THE SUBTROPICAL JET DISCUSSED ABOVE. GAP WINDS... A LATE SEASON STRONG COLD FRONT THAT JUST ENTERED THE GULF OF MEXICO IS EXPECTED TO SURGE SWD INTO THE BAY OF CAMPECHE SPREADING COOLER AIR INTO THE GULF OF TEHUANTEPEC BY MON NIGHT. NWP MODELS ARE IN GOOD AGREEMENT IN DEPICTING A GALE EVENT BEGINNING IN THE VICINITY OF TUE 0600 UTC. HOWEVER... GUIDANCE AND CLIMATOLOGY SUGGESTS THAT THE EVENT SHOULD BE FAIRLY SHORT LIVED. $$ CANGIALOSI