000 AXPZ20 KNHC 261600 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC WED MAR 26 2008 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 1515 UTC. ...ITCZ... ITCZ AXIS ALONG 3N78W 3N100W 6N120W 5N140W. SCATTERED MODERATE TO STRONG WITHIN 90-120 NM OF AXIS BETWEEN 97W AND 107W. SCATTERED MODERATE ISOLATED STRONG WITHIN 90-120 NM OF AXIS W OF 125W. SCATTERED MODERATE WITHIN 120 NM OF AXIS BETWEEN 96W AND 107W...AND BETWEEN 110W AND 116W. ...DISCUSSION... E OF 110W...QUIKSCAT DATA HAS BEEN OUT SINCE 0800 UTC BUT BASED ON LOWERING SURFACE PRESSURES OVER MEXICO AND SELY RETURN FLOW OVER THE GULF OF MEXICO WINDS SHOULD HAVE ALREADY DIMINISHED BELOW GALE FORCE IN THE GULF OF TEHUANTEPEC THIS MORNING. THE EDGE OF A 0940 UTC ASCAT PASS INDICATED NE TO E WINDS OF 20 KT THROUGH THE GULF OF PAPAGAYO. THIS FLOW WILL INCREASE SOMEWHAT TO 20 TO 25 KT OVER THE NEXT COUPLE OF DAYS AS ELY TRADES INCREASE OVER THE CARIBBEAN. NELY SWELL FROM BOTH TEHUANTEPEC AND PAPAGAYO IS COMBINING WITH SW CROSS EQUATORIAL SWELL TO CREATE AREAS OF CONFUSED SEAS GENERALLY 85-95W N OF 5N. FURTHER EAST...SHIP OBSERVATIONS N OF PANAMA BACKUP MODEL ANALYSIS HINTING OF FRESH NLY FLOW THROUGH THE GULF OF PANAMA. AT THE UPPER LEVELS UPPER DIVERGENCE ALONG A DEFORMATION ZONE ON THE SOUTH SIDE OF A BROAD UPPER RIDGE CENTERED NEAR 7N92W IS ENHANCING CONVECTION ALONG THE ITCZ BETWEEN 97W AND 107W. OTHER THAN ITCZ CONVECTION THE AREA WAS MARKED BY MODERATE TO STRONG SUBSIDENCE. W OF 110W...AN UPPER TROUGH N OF 20N ALONG 135W WITH A WELL DEFINED CYCLONIC CIRCULATION NEAR 27N135W WILL GRADUALLY SHIFT E AND DAMPEN OUT OVER THE NEXT COUPLE OF DAYS AS IT RIDES OVER A VERY BROAD LOW AMPLITUDE UPPER RIDGE CENTERED ALONG 110W/W MEXICO. AT THE SURFACE...1031 MB SURFACE HIGH PRES NEAR 35N144W WILL STRENGTHEN SLIGHTLY BEHIND THE UPPER SHORT WAVE AND SHIFT SLOWLY EWD THROUGH THU. THE SURFACE HIGH WILL MAINTAIN MODERATE NE TO E TRADES TO THE SOUTH...AND PROMPT AN AREA OF FRESH NLY WINDS ALONG THE NRN BAJA COAST. MEANWHILE NW SWELL CONTINUE TO PROPAGATE INTO THE AREA AND WILL COMBINE WITH CROSS EQUATORIAL SW SWELL GENERALLY S OF 15N. FURTHER S...AN ELONGATED UPPER RIDGE AXIS EXTENDS ALONG 8N. UPPER LEVEL DEFORMATION ZONE ON THE SOUTH SIDE OF THE RIDGE AXIS IS ENHANCING CONVECTION ALONG THE ITCZ AS DESCRIBED ABOVE. GLOBAL MODELS INDICATE THIS WILL PERSIST OVER THE NEXT COUPLE OF DAYS ALTHOUGH THE EXACT LOCATIONS ALONG THE ITCZ REMAIN UNCERTAIN. $$ COBB