000 AXPZ20 KNHC 261525 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC TUE SEP 26 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 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1500 UTC. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 8N82W 12N109W 10N120W 8N140W. SCATTERED MODERATE CONVECTION IS WITHIN 180 NM S OF THE AXIS BETWEEN 98W-105W. SCATTERED MODERATE/ISOLATED STRONG IS ALSO WITHIN 180 NM S OF THE AXIS BETWEEN 129W-136W. TROPICAL WAVES/LOW PRESSURE... A 1007 MB LOW IS CENTERED NEAR 14N115W MOVING W 5-10 KT. THE LOW LEVEL CIRCULATION CENTER IS ON THE ERN EDGE OF SCATTERED MODERATE CONVECTION WHICH IS MOST ORGANIZED IN A BANDED FEATURE FROM 12N-18N BETWEEN 115W-120W. OVERALL...THIS LOW HAS CHANGED LITTLE IN ORGANIZATION OVER THE PAST 24 HOURS AND APPEARS TO STILL BE FEELING EFFECTS OF EASTERLY SHEAR. ...DISCUSSION... A WELL DEFINED MID TO UPPER LEVEL TROUGH COVERS THE NW PORTION OF THE AREA FROM AN UPPER LOW NEAR THE CENTRAL CALIFORNIA COASTLINE TO A MORE VIGOROUS UPPER LOW NEAR 29N138W. SOME MOISTURE IS ASSOCIATED WITH THE WESTERN UPPER LOW...BUT LITTLE...IF ANY...IS DEEP IN NATURE. OTHERWISE FAIRLY DRY STABLE CONDITIONS EXIST BENEATH THE UPPER TROUGH. A MID-LEVEL RIDGE LIES TO THE SOUTH OF THE TROUGH EXTENDING FROM AN ANTICYCLONE OVER WRN MEXICO NEAR 22N105W WITH RIDGING EXTENDING TO NEAR 15N125W. ANOTHER ANTICYCLONE IS LOCATED JUST W OF THE DISCUSSION AREA NEAR 11N145W. A SLIGHT MID-UPPER LEVEL WEAKNESS EXISTS BETWEEN THESE MID-UPPER LEVEL HIGHS. A WEAKENING 40-60 KT SUBTROPICAL JET LIES BETWEEN THE TROUGH AND RIDGE. A SMALL UPPER LEVEL LOW IS SEEN SPINNING ON WATER VAPOR IMAGES NEAR 11N96W. ASSOCIATED SUBSIDENCE BENEATH THIS FEATURE MAY BE A CONTRIBUTING FACTOR IN THE LIMITED CONVECTION MOST EVERYWHERE ALONG THE WRN CENTRAL AMERICAN COAST. THE MOST ACTIVE WEATHER IN THE REGION IS IN THE EASTERN PORTION ASSOCIATED WITH THE 1007 MB LOW DISCUSSED ABOVE. UPPER DIVERGENCE ON THE SW PERIPHERY OF THE RIDGE OVER WRN MEXICO IS AIDING CONVECTIVE DEVELOPMENT NEAR THE SFC LOW. SE WINDS TO 20 KT ARE OCCURRING E OF THE LOW. THIS LOW WILL ENCOUNTER INCREASED SW SHEAR AS IT MOVES INTO THE WEAKNESS BETWEEN THE UPPER ANTICYCLONES AS DISCUSSED ABOVE...THEREFORE STRENGTHENING DOES NOT APPEAR LIKELY IN THE SHORT TERM. BESIDES FOR THE CONVECTION ASSOCIATED WITH THE SFC LOW...SCATTERED SHOWERS AND TSTMS EXIST ON THE S SIDE OF THE RIDGE FROM 13N-23N BETWEEN 104W-112W. AT THE SURFACE...MODERATE TO FRESH NLY GAP WINDS PERSIST THROUGH THE GULF OF TEHUANTEPEC TODAY AS HIGH PRESSURE BUILDS BEHIND A COLD FRONT TO THE N IN THE GULF OF MEXICO. THIS ACTIVITY IS EXPECTED TO PERSIST FOR THE NEXT COUPLE OF DAYS THEN DIMINISH AS THE HIGH PRESSURE WEAKENS AND SHIFTS E. S OF 10N...MODERATE TO FRESH CROSS EQUATORIAL FLOW CONTINUES ACCOMPANIED BY LARGE SWELL...PRIMARILY BETWEEN 92W AND 130W. $$ CANGIALOSI