000 AXPZ20 KNHC 180222 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC SUN APR 18 2010 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 0000 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 0215 UTC. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 05.5N77W TO 06.5N81W TO 05.5N89W TO 08.5N100W TO 06N116W TO 09N132W TO 07.5N140W. ISOLATED MODERATE TO STRONG CONVECTION WITHIN 150 NM S OF AXIS BETWEEN 98W AND 103W. ISOLATED MODERATE TO STRONG CONVECTION BETWEEN 210 AND 420 NM S OF AXIS BETWEEN 115W AND 122W. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION WITHIN 150 NM EITHER SIDE OF AXIS BETWEEN 123W AND 130W. ...DISCUSSION... A WELL DEFINED UPPER LEVEL CYCLONIC VORTEX EMBEDDED IN A HIGH AMPLITUDE TROUGH IS OBSERVED ON SATELLITE WATER VAPOR IMAGERY TO BE NEAR 29N136W. THE RESULTING SURFACE FEATURE IS A RATHER COMPLEX SYSTEM WITH TWO LOW CENTERS...ONE N OF THE AREA NEAR 32N136W WITH COLD FRONT EXTENDING FROM THE LOW ACROSS THE FORECAST AREA FROM 30N133W TO 25N133W TO 21N138W. NEAR GALE FORCE WINDS ARE WITHIN 240 NM E OF THIS COLD FRONT. THE SECOND LOW IS OVER THE NW PART OF THE FORECAST AREA NEAR 26N138W WITH COLD FRONT FROM THE LOW TO 26N136W TO 25N135W TO 22N140W. NEAR GALE FORCE WINDS ARE WITHIN 420 NM OF THE SOUTHERN QUADRANT OF THE LOW. AN UPPER LEVEL ANTICYCLONE IS CENTERED NEAR 09N118W WITH A HIGHLY AMPLIFIED RIDGE EXTENDING N TO WELL BEYOND THE AREA TO OVER THE WESTERN U.S. AND RESULTING BROAD ANTICYCLONIC CIRCULATION COVERING THE AREA E OF THE UPPER TROUGH MENTIONED IN THE PREVIOUS PARAGRAPH TO 100W. EAST OF THIS UPPER LEVEL ANTICYCLONE...A HIGH AMPLITUDE TROUGH PREVAILS WITH AXIS EXTENDING FROM THE CENTRAL GULF OF MEXICO SWD ACROSS SE MEXICO AND GUATEMALA...INTO THE E PACIFIC TO 00N90W. ELSEWHERE AT THE SURFACE...A WEAKENING 1018 MB HIGH IS CENTERED NEAR 26N122W. AS A RESULT OF THE WEAKENED HIGH...THE PRESSURE GRADIENT BETWEEN THE HIGH AND LOWER PRESSURE OF THE ITCZ HAS RELAXED...AND TRADES HAVE DIMINISHED BELOW 20 KT. WITH THE DECREASE IN TRADES...MOISTURE CONVERGENCE INTO THE ITCZ HAS DECREASED. AS A RESULT...CONVECTION W OF 113W HAS DECREASED SIGNIFICANTLY COMPARED TO THE PAST COUPLE OF DAYS. ITCZ CONVECTION BETWEEN 90W AND 100W HAS ALSO DECREASED SIGNIFICANTLY AS THIS AREA NOW LIES UNDER SUBSIDENT AIR ON THE W SIDE OF THE UPPER LEVEL TROUGH AXIS MENTIONED IN THE SECOND PARAGRAPH. $$ AL