000 AXPZ20 KNHC 162215 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC SUN SEP 16 2007 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2200 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 99W N OF 8N MOVING W 5-10 KT. A 1010 MB LOW IS ON THE WAVE AXIS NEAR 11N. THE LOW IS EXHIBITING A WELL-DEFINED WHAT APPEARS TO BE A MID LEVEL ROTATION ON SATELLITE IMAGERY. SCATTERED MODERATE/ISOLATED STRONG IS WITHIN 30 NM EITHER SIDE OF LINE 13N96.5W 13N99W 12N101W. THIS SYSTEM HAS THE POTENTIAL FOR SOME DEVELOPMENT OVER THE NEXT 48 HRS AS IT TRACKS IN A WNW DIRECTION. TROPICAL WAVE ALONG 112W FROM 8N-19N IS MOVING W ABOUT 7 KT. A WEAK 1010 MB LOW IS ON THE WAVE AXIS NEAR 15N. THE LOW IS RATHER SMALL...AND REMOVED FROM THE DEEP CONVECTION. THE DEEP CONVECTION IS COMPOSED OF THE SCATTERED MODERATE TYPE INTENSITY WITHIN 120-180 NM N OF THE LOW WITHIN 45 NM OF 18N111W...AND IS MOVING RAPIDLY WNW. THIS SYSTEM IS UNDER ELY SHEAR WHICH IS NOT ALLOWING CONVECTION ASSOCIATED WITH IT TO ORGANIZE. ...ITCZ... INTERTROPICAL CONVERGENCE ZONE...9N85W 11N100W 14N112W 14N122W 12N130W 10N140W. SCATTERED STRONG CONVECTION IS WITHIN 60 NM OF THE AXIS BETWEEN 120W-123W. SCATTERED MODERATE/ISOLATED STRONG CONVECTION IS WITHIN 120 NM S OF THE AXIS BETWEEN 102W-105W. SCATTERED MODERATE CONVECTION IS WITHIN 120 NM S OF THE AXIS BETWEEN 85W-89W. ...DISCUSSION... E OF 115W... WEAK ANTICYCLONIC OUTFLOW ALOFT OVER THE SW CARIBBEAN IS PROVIDING MODERATE NE SHEARING OVER THE WATERS S OF CENTRAL AMERICA. A WELL DEFINED UPPER LOW IS CENTERED OVER THE BAY OF CAMPECHE. A SMALL ANTICYCLONE IS TO THE S OF THE UPPER LEVEL LOW NEAR 13N96W. WITH THE CLOSE PROXIMITY OF THESE TWO FEATURES... DIVERGENCE ALOFT IS BEING NOTED S OF THE GULF OF TEHUANTEPEC TO 13N AND E OF THE WAVE ALONG 99W. THIS IS ALLOWING FOR CONVECTION ASSOCIATED WITH THE LOW AND WAVE ALONG 99W MENTIONED ABOVE TO CONTINUE TO FLARE UP. MODERATE TO STRONG SHEARING IS EVIDENT BETWEEN THE UPPER LOW OVER THE BAY OF CAMPECHE AND AN UPPER RIDGE OVER CENTRAL MEXICO. MODERATE TO STRONG NE SHEAR IS EVIDENT S OF 7N E OF 94W. THIS AS STATED ABOVE UNDER TROPICAL WAVE ALONG 112W IS KEEPING CONVECTION ALONG AND NEAR THE ITCZ TO A MINIMUM. A WEAK PRES PATTERN PREVAILS AT THE SURFACE. W OF 115W... BROAD UPPER ANTICYCLONE CENTERED NEAR 23N117W IS CONTINUING THE MODERATE TO STRONG ELY SHEAR ACROSS THE ITCZ. THE UPPER RIDGE AXIS EXTENDS FROM CENTRAL MEXICO TO THE CENTER OF THE UPPER ANTICYCLONE TO 16N140W...AND SW TO OUTSIDE THE REGION AT 15N144W. UPPER DIVERGENCE ON THE SW PERIPHERY OF THE UPPER ANTICYCLONE IS AIDING CONVECTION NEAR THE ITCZ BETWEEN 120W-130W. A WEAK AND ELONGATED 1009 MB LOW IS AT THE SURFACE NEAR 13N127W. A TROUGH EXTENDS NE FROM THE LOW THROUGH 15N124W TO 11N122W. THE LOW IS FORECAST TO MOVE IN A NW DIRECTION OVER THE NEXT 24 HRS AND REMAIN RATHER WEAK. FRESH NELY WINDS ARE EVIDENT N OF THE ITCZ BETWEEN THE LOW PRES AND STRONG HIGH WELL TO THE N. AT THE SURFACE...A RIDGE EXTENDS INTO THE AREA THROUGH 32N133W...AND REACHES TO 16N117W. HIGH PRES COVERS THE AREA N OF 20N W OF 118W. SCATTERED PATCHES OF STRATOCUMULUS CLOUDS WITH POSSIBLE ISOLATED SHOWERS ARE NW OF LINE 14N140W 20N128W TO 32N121W. $$ AGUIRRE