000 AXPZ20 KNHC 150920 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1005 UTC TUE SEP 15 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 0845 UTC. ...SPECIAL FEATURE... A SURFACE LOW 16N111W 1008 MB MOVING WNW 8 KT. LOW IS PART OF A LARGE AREA OF LOW PRESSURE THAT EXTENDS OUT ABOUT 400 NM FROM THE POINT 15N113W. UPPER DIFFLUENT FLOW IS CONTRIBUTING TO THE LOW LEVEL CONVERGENCE THAT IS INCREASING THE CYCLONIC CIRCULATION IN THE LOW LEVELS. WIDESPREAD MULTI LEVEL CLOUDS AND EMBEDDED AREAS OF CONVECTION ARE WITHIN THIS AREA. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 150 NM IN THE NORTH QUADRANT OF THE LOW. IT IS POSSIBLE THAT A TROPICAL CYCLONE MAY FORM WITHIN THIS BROAD AREA OR THE LOW ITSELF MAY DEVELOP INTO A TROPICAL CYCLONE OVER THE NEXT 48 HOURS. ...TROPICAL WAVE... TROPICAL WAVE ALONG 106W FROM 08N TO 18N MOVE WEST 15 KT. NO CONVECTION IS NEAR THE WAVE AT THIS TIME. TROPICAL WAVE ALONG 120W FROM 08N TO 16N MOVE WEST 15 KT. SOME CONVECTION IS NEAR THE WAVE IN THE ITCZ. THE CONVECTION IS NOT ORGANIZED BY CYCLONIC FLOW. ...THE ITCZ... THE INTERTROPICAL CONVERGENCE ZONE IS ALONG THE LINE 07N77W TO 09N100W TO 10N120W TO 06N140W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 60 NM EITHER SIDE OF THE ITCZ AXIS E OF 80W. SCATTERED MODERATE CONVECTION IS WITHIN THE AREA 60 NM EITHER SIDE OF A LINE FROM 14N112.5W TO 10N121W. ...DISCUSSION... TROUGH OVER THE SOUTHWEST UNITED STATES EXTENDS OVER NORTHWEST MEXICO AND THE NORTHEAST PART OF THE PACIFIC OCEAN NORTH OF 25N EAST OF 123W. CLOUDS IN THIS ARE ARE BROKEN TO OVERCAST STRATOCUMULUS OVER THE OCEAN AND THE COASTAL AREAS OF BAJA CALIFORNIA. THE TROUGH IS FORECAST TO REMAIN OVER THE SOUTHWEST UNITED STATES AND CONTINUE TO BE OVER NORTHERN MEXICO THROUGH THE NEXT SEVERAL DAYS. A STRONG MIDDLE LATITUDE TROUGH IS MOVING OVER THE FAR NORTHWEST PART OF THE AREA. THE TROUGH IS FORECAST TO REMAIN MOSTLY NORTH OF THE AREA AND TO PULL FURTHER NORTH AFTER A COUPLE OF DAYS. SOME MULTI LEVEL LAYERED CLOUDINESS IS ASSOCIATED WITH THE TROUGH BUT THESE CLOUDS ARE EXPECTED TO REMAIN MOSTLY NORTH OF 32N. BETWEEN THE TWO TROUGHS A SHARP RIDGE EXTENDS NORTH OF 25N. THIS RIDGE IS PART OF A LARGE ANTICYCLONIC FLOW THAT COVERS MOST OF THE PACIFIC REGION. THE RIDGE EXTENDS EAST TO A LINE FROM NORTHWESTERN YUCATAN PENINSULA TO THE ITCZ NEAR 100W. THIS RIDGE IS DIFFLUENT ALOFT TO THE SOUTH OF A LINE THAT EXTENDS FROM NEAR 25N105W TO THE ITCZ AT 140W. NORTHWEST OF THE LINE MIDDLE AND UPPER LEVEL SUBSIDENCE IS KEEPING THE MIDDLE AND UPPER LEVELS DRY AND CLOUD FREE. BROKEN TO OVERCAST STRATOCUMULUS ARE WITHIN THIS AREA NORTH OF 20N. THE DIFFLUENT AREA INCLUDES THE SPECIAL FEATURES AREA AND ALSO WIDESPREAD MULTI LEVEL CLOUDINESS NEAR THE ITCZ WEST OF 125W. WEAK SURFACE RIDGE IS NORTH OF 23N FROM 118W TO 135W. ELSEWHERE EXCEPT FOR THE BROAD LOW A WEAK FLAT PRESSURE GRADIENT IS ANALYZED. $$ LL