000 AXPZ20 KNHC 031009 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC SAT OCT 03 2009 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 0915 UTC. ...SPECIAL FEATURE... NEW DOWNGRADED TROPICAL DEPRESSION OLAF WAS CENTERED NEAR 24.1N 117.2W AT 03/0900 UTC OR ABOUT 405 NM...750 KM...WEST OF THE SOUTHERN TIP OF BAJA CALIFORNIA...MOVING N OR 010 DEG AT 3 KT. MAXIMUM SUSTAINED WIND SPEED WAS 30 KT WITH GUSTS TO 40 KT. ESTIMATED MINIMUM CENTRAL PRESSURE IS 1005 MB. SOUTHERLY SHEAR OF NEAR 25 KT CONTINUES TO TAKE ITS TOLL ON OLAF WITH THE MID LEVEL CIRCULATION AND DEEP CONVECTION 90-120 NM OFF TO THE NE OF THE LOW LEVEL CENTER. RECENT MICROWAVE PASSES HAVE BEEN VERY HELPFUL IN LOCATING THE EXPOSED LOW LEVEL CENTER...AND THE OFFICIAL CENTER OF OLAF HAS BEEN RELOCATED...AGAIN...TO THE SW OF OUR PREVIOUS POSITIONS. THE SHEAR IS FORECAST TO INCREASE FURTHER AND THIS COMBINED WITH A TRACK TOWARD BAJA CALIFORNIA OVER COOLER WATERS SHOULD RESULT IN THE DISSIPATION OF THE REMNANT LOW WITHIN THE NEXT 36 TO 48 HOURS. ADDITIONAL INFORMATION CAN BE FOUND UNDER AWIPS/WMO HEADERS MIATCMEP3/WTPZ23 KNHC. ...ITCZ... AXIS WAS CENTERED ALONG 09N78W TO 07N89W TO 08N108W TO 11N115W WHERE IT BECOMES DISCONTINUED. ITCZ RESUMES AT 16N123W TO 11N133W TO 10N140W. SCATTERED MODERATE WITHIN 120 NM S OF THE AXIS E OF 88W. SCATTERED MODERATE WITHIN 90 NM N AND 120 NM S OF ITCZ AXIS W OF 130W. ...DISCUSSION... AN OMEGA BLOCKING PATTERN PERSISTS ACROSS THE SUBTROPICS BETWEEN THE E COAST OF THE U.S. AND 160W. AN AMPLIFIED POSITIVELY TILTED UPPER PATTERN REMAINS IN PLACE S OF 38N WITH A SHEAR AXIS EXTENDING FROM A S/W TROUGH MOVING INTO THE W COAST OF THE U.S. AND SWEEPING ACROSS CALIFORNIA... SOUTHWESTWARD THROUGH 31N127W TO A BROAD AND QUASISTATIONARY CYCLONIC CIRCULATION JUST W OF THE AREA NEAR 25N144W. THE BASE OF THIS TROUGH EXTENDED S TO NEAR 16N147W...WITH BROAD CYCLONIC CURVATURE OCCURRING BETWEEN 136W AND 152. SATELLITE DERIVED WINDS INDICATED A 60-80 KT JET LIFTING OUT OF THE E SIDE OF THE BROAD TROUGH AND INTO THE BASE OF THE S/W MOVING ACROSS SRN CALIFORNIA. THIS JET WAS ADVECTING SHEARED UPPER LEVEL MOISTURE AND OUTFLOW FROM ITCZ CONVECTION W OF 130W AND FROM OLAF...SPREADING IT NORTHEASTWARD OVER MEXICO AND INTO THE SW CONUS. MODERATE TO STRONG SUBSIDENCE WITH DRY STABLE AIR IN THE MIDDLE AND UPPER LEVELS OF THE ATMOSPHERE WAS NOTED WITH AND BEHIND THE S/W MOVING ACROSS SRN CALIFORNIA...AND ALSO THROUGH THE BASE OF THE BROAD TROUGH ALONG 144W. DOWNSTREAM...A BROAD UPPER LEVEL ANTICYCLONIC CIRCULATION WAS CENTERED MEXICO NEAR 22N101W...WITH A BROAD AND RELATIVELY FLAT RIDGE TO THE N FROM THE NORTHERN COAST OF THE BAJA PENINSULA INTO SW TEXAS. OLAF REMAINS SITUATED IN THE FAR WESTERN PERIPHERY OF THIS ANTICYCLONE AND CONTINUES TO ENDURE SSW SHEAR. A MID TO UPPER LEVEL CYCLONE WAS STRADDLING THE EQUATOR ALONG 116W WITH TROUGH EXTENDING NW TO 12N122W. DRY AND SUBSIDENT AIR E OF THIS TROUGH WAS S OF 07N AND E OF 110W...WHILE TO THE W OF THE TROUGH AND W OF 128W...UPPER DIVERGENCE WAS MAINTAINING ACTIVE CONVECTION ALONG THE ITCZ. DOWNSTREAM OF THE UPPER RIDGE...NLY FLOW ALOFT WAS SPILLING INTO THE N SIDE OF A TUTT AXIS ALONG 15N AND ACROSS CENTRAL AMERICA...THAT EXTENDING INTO A TUTT LOW CENTERED ACROSS JAMAICA. THIS WAS PRODUCING SUBSIDENT CONDITIONS ACROSS MUCH OF CENTRAL AMERICA FROM 14N TO 18N...WHILE RELATED CONVERGENCE ALOFT WAS OCCURRING ALONG AND OFFSHORE OF THE W COAST OF MEXICO S OF 20N. AT THE SURFACE... STRONG RIDGE OF HIGH PRES EXTENDED SE FROM A 1034 MB HIGH NEAR 39N146W AND COVERED THE DISCUSSION AREA N OF 18N W OF 122W... WHERE BROKEN TO LOCALLY OVERCAST STRATOCUMULUS PREVAILED. THE RIDGE COMBINED WITH THE LOWER PRESSURES IN THE TROPICS AND W OF TROPICAL DEPRESSION OLAF AND CONTINUED TO RESULT IN A LARGE AREA OF NE TRADES OF 20-25 KT NW OF A LINE FROM 30N122W TO 20N123W TO 13N140W WITH CONFUSED SEAS 8 TO 11 FT IN A BROAD MIX OF SWELL. THESE WINDS ARE FORECAST TO DIMINISH IN ABOUT 48 HOURS AS A WEAKENING FRONTAL BOUNDARY DROPS S TO ALONG THE FAR NRN PORTION AND WILL BREAK DOWN THE RIDGE ENOUGH TO LESSEN THE SUPPORTING PRESSURE GRADIENT. SWELLS THROUGHOUT THIS AREA WILL GRADUALLY SUBSIDE OVER MUCH OF THE WRN PORTION BUT REMAIN UP TO 11 FT OVER THE WRN PORTION WITH PERIODS OF 9-11 SEC. OVER THE SRN PORTION OF THE AREA SEAS OF 8 TO 10 FT IN SLY SWELL DUE TO LONG PERIOD SRN HEMISPHERIC SWELLS FROM OVER THE PAST SEVERAL DAYS SHOULD SLOWLY SUBSIDE DURING THE NEXT 2 TO 3 DAYS AS ASSOCIATED STRONG SRN HEMISPHERIC FRONTAL SYSTEMS PROGRESS SWD. $$ STRIPLING