000 AXPZ20 KNHC 050328 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC SAT MAY 05 2007 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 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0315 UTC. ...ITCZ... AXIS ALONG 7N78W 10N94W 7N110W 9N120W 3N140W. SCATTERED MODERATE TO STRONG WITHIN 120-180 NM EITHER SIDE OF AXIS BETWEEN 110W AND 117W...AND WITHIN 60 NM EITHER SIDE OF LINE 12.5N105W 11N110W. SCATTERED MODERATE WITHIN 90 NM EITHER SIDE OF AXIS BETWEEN 92W AND 101W. ...DISCUSSION... N OF 20N...HIGHLY AMPLIFIED PATTERN IN PLACE WITH REX BLOCK FEATURE JUST NW OF DISCUSSION AREA BETWEEN 140W AND 145W CONSISTING OF A DRY MID/UPPER LOW CYCLONIC CIRCULATION NEAR 26N146W...AND UPPER RIDGE TO THE N AND NE. ASSOCIATED 1029 MB SFC HIGH IS CENTERED NEAR 34N143W. MOST RECENT SHIP OBSERVATIONS SHOW A CONTINUATION OF FRESH TO STRONG TRADES ON THE SOUTHERN PERIPHERY OF THE HIGH AS FAR S AS 8N. TO THE EAST OF THE UPPER RIDGE...A BROAD MID TO UPPER LEVEL TROUGH DIGGING INTO THE NORTHERN ROCKIES IS PROVIDING UPPER SUPPORT TO A 1000 MB SURFACE LOW PRESSURE SYSTEM OVER CALIFORNIA AND ASSOCIATED COLD FRONT MOVING FROM THE SOUTHERN CALIFORNIA COAST INTO THE DISCUSSION AREA ALONG 31N. THE TIGHT GRADIENT BETWEEN THE SURFACE HIGH PRES TO THE W AND THE LOW OVER CALIFORNIA HAS SET UP A GOOD NW FETCH OF GALE FORCE WINDS WITH LARGE NLY SWELLS OF UP TO 13 FT NOW MOVING INTO THE NE PART OF THE AREA. FRESH TO STRONG NWLY WINDS OF 20-25 KT ARE EXTENDING SWD ALONG THE BAJA COAST ON THE EASTERN EDGE OF THE HIGH PRES. LITTLE CHANGE IS EXPECTED IN CONDITIONS THROUGH SAT AS THE RIDGE REMAINS IN PLACE. HOWEVER...THE UPPER RIDGE WILL WEAKEN BY LATE SAT...AHEAD OF A DEEP UPPER TROUGH ADVANCING THROUGH THE CENTRAL PACIFIC...ALLOWING THE SURFACE RIDGE TO WEAKEN SLIGHTLY. THE NW FLOW OFF OF BAJA WILL SUBSEQUENTLY DIMINISH WITHIN 36 HOURS ...AS WILL TRADE FLOW S OF THE RIDGE. S OF 20N...UPPER TROUGH EXTENDS FROM THE SW N ATLANTIC SOUTHWEST THROUGH THE CENTRAL BAHAMAS...W CARIBBEAN TO THE EAST PACIFIC NEAR 10N88W. FAIRLY DRY MID LEVEL AIR ASSOCIATED WITH THE UPPER TROUGH IS SUPPRESSING CONVECTION OVER THE EAST PACIFIC. HOWEVER...UPPER DIVERGENCE E OF THE UPPER TROUGH IS ENHANCING CONVECTION OFF THE COLOMBIAN COAST AND GULF OF PANAMA. FURTHER W...UPPER LEVEL ANTICYCLONE CENTERED NEAR 11N120W IS SIMILARLY AIDING CONVECTION ALONG AND N OF THE ITCZ BETWEEN 110W AND 117W. $$ COBB