000 AXPZ20 KNHC 131537 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC THU SEP 13 2007 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 1500 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 79W N OF 7N IN THE BAY OF PANAMA MOVING W 5 OT 10 KT. CONVECTION IS FLARING ON THE SOUTHERN END OF THE WAVE...GENERALLY N OF 6N AND W OF 80W. THE CONVECTION IS INTERACTING WITH THE COLOMBIAN PACIFIC COAST AND IS FURTHER ENHANCED BY SLY DIVERGENT FLOW ALOFT. TROPICAL WAVE ALONG 106W MOVING W 5-10 KT WITH A WEAK 1009 MB LOW ALONG THE AXIS NEAR 9N. THE FIRST VISIBLE IMAGES OF THE DAY SHOW BROAD LOW LEVEL TURNING AROUND THE LOW. CONVECTION REMAINS FAIRLY LIMITED HOWEVER. TROPICAL WAVE ALONG 135W S OF 15N MOVING W 10 KT. A WEAK CIRCULATION IS ASSOCIATED WITH THIS WAVE WHERE IT INTERSECTS WITH THE ITCZ NEAR 11N. HOWEVER...NO SIGNIFICANT CONVECTION IS NOTED. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 8N83W 8N90W 13N101W 9N110W 11N114W 13N122W 10N140W. SCATTERED MODERATE CONVECTION WITHIN 240 NM OF AXIS BETWEEN 93W AND 101W. SCATTERED MODERATE WITHIN 90 NM N OF AXIS BETWEEN 107W AND 111W. ...DISCUSSION... E OF 115W... MODERATE TO FRESH SWLY CROSS EQUATORIAL FLOW IS PROVIDING SUFFICIENT LOW LEVEL CONVERGENCE TO SUPPORT THE SCATTERED MODERATE CONVECTION NOTED ABOVE ALONG THE ITCZ FROM 93W TO 101W. ELY SHEAR IS IMPACTING THIS CONVECTION S OF AN UPPER ANTICYCLONE EXTENDING ACROSS CENTRAL MEXICO. AN UPPER TROUGH IS SITUATED W OF THIS UPPER ANTICYCLONE AND S OF BAJA FROM 24N107W TO AS FAR SOUTH AS 14N112W. UPPER DIVERGENCE ON THE E SIDE OF THE TROUGH IS ENHANCING CONVECTION WITHIN 90 NM E OF A SURFACE LOW 1010 MB CENTERED NEAR 17N112W. WHILE THE ROTATION IS BETTER DEFINED THAN BEFORE...CONVECTION IS NOT IMPRESSIVE SO FAR. WHILE GLOBAL MODELS ARE MIXED ON WHETHER THIS WILL SIGNIFICANTLY DEVELOP OVER THE NEXT COUPLE OF DAYS...ANY DEVELOPMENT WILL BE SLOW. W OF 115W... AN UPPER ANTICYCLONE OFF THE W COAST OF CENTRAL BAJA NEAR 26N116W.UPPER RIDGE AXIS EXTENDS FROM THE UPPER ANTICYCLONE OFF CENTRAL BAJA TO 20N140W. AN UPPER TROUGH EXTENDS S OF THIS UPPER RIDGE AXIS FROM 20N 11N ALONG 126W. A SURFACE LOW 1010 MB IS CENTERED ALONG THE ITCZ NEAR 15N120W. CONVERGENCE AROUND THIS FEATURE ALONG WITH SOME MINOR UPPER ENHANCEMENT IS SPARKING SCATTERED GENERALLY LIGHT CONVECTION WITHIN 120 NM OF THE CENTER OF THE LOW. HOWEVER...GLOBAL MODELS DO NOT SHOW SIGNIFICANT DEVELOPMENT OF THIS SYSTEM AS IT HEADS INTO A MORE UNFAVORABLE ENVIRONMENT FURTHER TO THE NW. ELSEWHERE...DRY AIR ALONG WITH NWLY FLOW ALOFT ON THE THE SOUTH SIDE OF THE UPPER RIDGE AXIS ARE SUPPRESSING SIGNIFICANT CONVECTIVE DEVELOPMENT OVER THE REMAINDER OF THE AREA. AT THE SURFACE...HIGH PRES 1021 MB IS CENTERED NEAR 29N129W. MODERATE FRESH N AND NE WINDS ARE EVIDENT IN SCATTEROMETER AND SHIP DATA BETWEEN THE SURFACE HIGH AND LOW PRES ASSOCIATED WITH THE ITCZ AND TROPICAL WAVES...AND IS EXPECTED TO PERSIST FOR AT LEAST THE NEXT 48 HOURS. $$ CHRISTENSEN