000 AXPZ20 KNHC 111525 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC TUE JUL 11 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. ...SPECIAL FEATURES... .TROPICAL STORM BUD NEAR 13.9N 112.6W 1005 MB AT 1500 UTC MOVING WNW OR 285 DEG AT 8 KT. MAXIMUM SUSTAINED WINDS 35 KT GUSTS 45 KT. TROPICAL STORM FORCE WINDS WITHIN 30 NM OF CENTER EXCEPT 10 NM NW QUADRANT. SEAS 12 FT OR GREATER WITHIN 30 NM OF CENTER WITH SEAS TO 15 FT. SEE LATEST NHC FORECAST/ADVISORY UNDER AWIPS/WMO HEADERS MIATCMEP3/WTPZ23 KNHC FOR MORE DETAILS. A LARGE AREA OF CONVECTION IS OVER THE SOUTH SEMICIRCLE AND EXTENDS OUT 200 NM. THE WATER VAPOR IMAGERY INDICATES SOME NORTHEASTERLY SHEAR OVER THE SYSTEM AND THIS IS PREVENTING AN MORE SYMMETRIC CONVECTION PATTERN. NUMEROUS MODERATE TO STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 12.5N112W. A 1008 MB LOW IS CENTERED NEAR 12N98W...ABOUT 250 NM S OF THE MEXICO COAST. THE LOW IS MOVING W 5-10 KT AND IS COLLOCATED WITH A TROPICAL WAVE THAT EXTENDS NORTH OF 5N ALONG 98W. THE BROAD CIRCULATION IS NOT WELL DEFINED. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 14.7N100W AND THIS CONVECTION IS MOVING WEST AWAY FROM THE CENTER. THIS IS NOT CONDUCIVE TO DEVELOPMENT. UPPER LEVEL OUTFLOW IS GOOD OVER THE SYSTEM. TROPICAL CYCLONE FORMATION IS POSSIBLE WITHIN THE NEXT 36 HRS. ...TROPICAL WAVES... TROPICAL WAVE ALONG 125W FROM 5N TO 17N MOVING W 5 KT WITH A 1010 MB LOW CENTERED NEAR 12N. A SMALL CLUSTER OF CONVECTION IS SOUTHWEST OF THE CENTER OF THE LOW. COOLER WATER TEMPERATURES AND ELY VERTICAL SHEAR WILL INHIBIT DEVELOPMENT. ..ITCZ... ITCZ AXIS IS CENTERED ALONG...4N77W 10N100W 10N115W 6N140W. SCATTERED MODERATE TO STRONG CONVECTION IS WITHIN 75 NM OF THE POINT 10N96.9W. ...DISCUSSION... MIDDLE AND UPPER LEVEL TROUGH IS NORTHWEST OF A LINE 32N118W TO 25N140W. A SMALL EMBEDDED CYCLONIC CIRCULATION CENTER IS NEAR 31N134W. THIS AREA IS DRY IN THE MIDDLE AND UPPER LEVELS AND IS CLOUD FREE IN THESE LEVELS WITH BROKEN TO OVERCAST STRATOCUMULUS IN THE LOWER LEVELS. THE REMAINDER OF THE AREA NORTH OF 15N IN THE MIDDLE AND UPPER LEVELS IS A RIDGE. SOUTH OF 15N BROAD TROUGH IS IN THE MIDDLE AND UPPER LEVELS. WEST OF A LINE 30N110W TO THE ITCZ NEAR 122W IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS. IN THE LOWER LEVELS BROKEN TO OVERCAST STRATOCUMULUS IS OBSERVED. EAST OF THIS LINE TO 95W THE ATMOSPHERE IS MOIST IN THE DEEP LAYER WITH MULTI LEVEL CLOUDS AND EMBEDDED AREAS OF CONVECTION. FROM 95W TO 85W THE ATMOSPHERE IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS. EAST OF 85W DEEP LAYER MOISTURE WITH MULTI LEVEL CLOUDS AND EMBEDDED AREAS OF CONVECTION IS NOTED. AT THE SURFACE NORTHWEST OF A LINE FROM 30N115W TO 7N140W A WEAK RIDGE IS ANALYZED. ELSEWHERE BROAD TROUGH IS OVER THE AREA. $$ LL