000 AXPZ20 KNHC 122123 TWDEP TROPICAL WEATHER DISCUSSION NWS NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC SAT MAY 12 2012 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 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2045 UTC. ...INTERTROPICAL CONVERGENCE ZONE/MONSOON TROUGH... MONSOON TROUGH EXTENDS FROM 11N86W TO 11N95W TO A 1008 MB LOW AT 10N105W TO A 1009 MB LOW AT 09N114W TO 06N119W AND THEN CONTINUES AS THE ITCZ TO 04N130W TO 04N140W. SCATTERED MODERATE ISOLATED STRONG CONVECTION IS LOCATED WITHIN 90 NM EITHER SIDE OF A 06N80W TO 04N87W LINE...WITHIN 60 NM EITHER SIDE OF A 07N91W TO 07N99W LINE...AND FROM 07 TO 10N BETWEEN 108W AND 113W. ...DISCUSSION... A LARGE AND WELL-DEFINED MIDDLE/UPPER LEVEL CYCLONIC CIRCULATION IS POSITIONED AT 30N133W AND IS MOVING NE. THE CIRCULATION HAS A DIAMETER OF ABOUT 12 DEGREES. THIS FEATURE IS FORECAST TO ACCELERATE OUT OF THE FORECAST AREA WITHIN THE NEXT 24 HOURS. MODERATE SOUTHWESTERLY WINDS ALOFT WILL COVER THE AREA W OF A 32N125W TO 20N125W TO 10N140W LINE AT DAY TWO. WATER VAPOR IMAGERY INDICATES STRONG SUBSIDENCE ALONG AND OFF THE COAST OF MEXICO AND ALSO IN THE LARGE AREA S OF 25N TO THE EQUATOR W OF 120W. AT THE SURFACE A STATIONARY 1022 MB HIGH IS CENTERED NEAR 25N128W. ALSO A WEAKENING 1016 MB LOW IS LOCATED NEAR 28N137W. WINDS ALOFT ARE GENERALLY LIGHT E OF 100W INTO CENTRAL AMERICA AND SOUTH AMERICA. ABUNDANT MOISTURE IS SEEN IN THE WATER VAPOR LOOP WITH SEVERAL AREAS OF DEEP CONVECTION. ONE IS AN AREA OF SCATTERED MODERATE TO STRONG CONVECTION WITHIN 60 NM EITHER SIDE OF A 09N99W TO 12N104W LINE IN ASSOCIATION WITH THE 1008 MB LOW AT 10N105W. ANOTHER IS AN AREA OF SCATTERED MODERATE TO STRONG CONVECTION WITHIN A 60 NM RADIUS OF 10N117W IN ASSOCIATION WITH THE 1009 MB LOW AT 09N114W. A GULF OF TEHUANTEPEC EVENT IS FORECAST IN 24 HOURS WITH WINDS NE 20 TO 25 KT AND SEAS TO 8 FT. $$ CAB