000 AXPZ20 KNHC 110320 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC TUE NOV 11 2008 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 0300 UTC. ...ITCZ... THE INTERTROPICAL CONVERGENCE ZONE AXIS LIES ALONG THE LINE 06N77W TO 06N110W TO 08N130W TO 06N140W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN 120 NM OF THE POINT 07.5N94W. SCATTERED MODERATE WITH ISOLATED STRONG CONVECTION IS WITHIN THE AREA FROM 06.5N TO 09.5N BETWEEN 127W AND 137W. ...DISCUSSION... A MAINLY UPPER TROUGH IS MOVING RAPIDLY EAST ACROSS THE NORTHEAST PART OF THE PACIFIC OCEAN AREA AND OVER NORTHERN MEXICO. LITTLE IN THE WAY OF CLOUDS IS ASSOCIATED WITH THE SYSTEM. A LONG LIVED MIDDLE AND UPPER TROUGH CONTINUES ALONG THE LINE FROM SOUTHERN TEXAS NEAR 30N97W TO 21N125W TO 07N140W. A PLUME OF UPPER LEVEL MOISTURE IS NOTED TO THE SOUTHEAST OF THE TROUGH AXIS. THE PLUME IS NEAR 300 NM WIDE EAST OF 115W AND 600 NM WIDE WEST OF 115W. THIS MOISTURE IS EMANATING FROM CONVECTION NEAR THE ITCZ WEST OF 125W. THE AREA NORTH AND WEST OF THE TROUGH AXIS IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS WITH BROKEN TO OVERCAST STRATOCUMULUS IN THE LOWER LEVELS NORTH OF ABOUT 19N. ITCZ CONVECTION FROM 89W TO 98W IS ADVECTING NORTHEAST IN THE MIDDLE AND UPPER LEVELS OVER THE ISTHMUS OF CENTRAL AMERICA. OTHERWISE SOUTH AND EAST OF A LINE FROM NEAR 22N98W TO 20N110W TO 06N118W TO 04N140W THE ATMOSPHERE IS DRY AND CLOUD FREE IN THE MIDDLE AND UPPER LEVELS. SOUTH OF THE ITCZ BROKEN TO OVERCAST STRATOCUMULUS IS NOTED ACROSS THE ENTIRE AREA. REMAINDER OF THE MIDDLE AND UPPER LEVELS IS ANALYZED AS A BROAD RIDGE. MODERATE RIDGE IS NORTH OF 12N WEST OF 110W. THE RIDGE IS FORECAST TO STRENGTHEN SOME IN THE NEXT 24 HOURS INCREASING THE NORTHEAST TRADES. WINDS IN THE AREA FROM 10N TO 25N WEST OF 120W WILL BE IN THE 20 TO 25 KT RANGE AND IN WITHIN THE NEXT 24 HOURS OCCASIONALLY TO 30 KNOTS. THE REMAINDER OF THE AREA IS ANALYZED AS A BROAD TROUGH. $$ LL