000 AXPZ20 KNHC 150331 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC THU JUN 14 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 2145 UTC. ...TROPICAL WAVES.. A TROPICAL WAVE IS N OF 3N ALONG 92W AND HAS BEEN MOVING W ABOUT 12 TO 15 KT OVER THE PAST 24 HOURS. ONLY A SLIGHT ENHANCEMENT OF CONVECTION WAS NOTED ALONG THE ITCZ E OF THE WAVE NEAR 10N91W. A TROPICAL WAVE ALONG 105.5W HAS MOVED W ABOUT 10 KT THE PAST 24 HOURS. A LARGE AREA OF CONVECTION WAS ENHANCED ALONG THE ITCZ...ROUGHLY FROM 8N TO 13N BETWEEN 104W AND 109W...BUT IS DECREASING IN INTENSITY AT THE MOMENT. A TROPICAL WAVE ALONG 117W HAS MOVED W 10 KT THE PAST 24 HOURS. CYCLONIC TURNING IS NOTED NEAR 7N116W...BUT A COUPLE OF TSTMS ACCOMPANY THE WAVE AT THE MOMENT. ..ITCZ... INTERTROPICAL CONVERGENCE ZONE...12N86W 12N95W 8N112W 10N118W 7N140W. SCATTERED MODERATE ISOLATED STRONG CONVECTION IS NOTED WITHIN 150 NM OF LINE 8N96W 15N104W. SCATTERED MODERATE CONVECTION IS OBSERVED WITHIN 60 NM 10N90W AND WITHIN 150 NM OF LINE 12N104W 8N113W. ...DISCUSSION... AN UPPER LEVEL TROUGH IS SLOWLY FILLING ALONG 32N101W 24N114W THROUGH A SMALL UPPER CYCLONE AT 18N113W WITH THE TROUGH CONTINUING SW THROUGH 10N120W LOSING IDENTITY NEAR THE EQUATOR AT 122W. AN UPPER LEVEL ANTICYCLONE CONTINUES TO DRIFT W AND IS CURRENTLY NEAR 27N147W WITH A RIDGE EXTENDING E TO NEAR 27N134W. ANOTHER UPPER ANTICYCLONE IS NEAR 26N123W. AN UPPER TROUGH IS NOTED ALONG 30N129W 24N130W INTO AN UPPER CYCLONE AT 15N137W...EFFECTIVELY SEPARATING THE TWO ANTICYCLONIC SYSTEMS DESCRIBED ABOVE. A LOW LEVEL RIDGE EXTENDS ALONG 32N137W TO 25N115W. THESE UPPER SYSTEMS COMBINE TO ADVECT DRY UPPER AIR OVER MOST OF THE DISCUSSION AREA N OF 12N W OF 116W. ANOTHER UPPER ANTICYCLONE IS W OF THE DISCUSSION AREA NEAR 12N146W WITH A RIDGE EXTENDING SE INTO THE DISCUSSION AREA AT 5N146W. UPPER DIFFLUENCE...FROM THE RIDGE AND THE CYCLONE JUST TO THE N...ENHANCED CONVECTION ALONG THE ITCZ BETWEEN 132W AND 145W. THE RESULTANT DEBRIS MOISTURE IS COVERING THE AREA S OF 10N W OF 131W. AN UPPER ANTICYCLONE IS CENTERED NEAR 12N81W AND ITS ENVELOPE OF ANTICYCLONIC FLOW IS DOMINATING THE UPPER LEVELS E OF 110W. A RIDGE EXTENDING W TO NEAR 11N117W LIES OVER THE ITCZ AND ENHANCED CONVECTION BETWEEN 95W AND 107W. THE RESULTANT DEBRIS MOISTURE IS ADVECTED N TO CENTRAL AMERICA...BUT SEEMS TO EVAPORATE ALONG 17N. DRY UPPER AIR IS NOTED S OF THE ITCZ... ROUGHLY S OF 6N E OF 132W. $$ FORECASTER NELSON