000 AXPZ20 KNHC 111538 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 1605 UTC FRI AUG 11 2006 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 1200 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 1515 UTC. ...TROPICAL WAVES... TROPICAL WAVE ALONG 100W S OF 16N MOVING W 15 TO 20 KT. THE WAVE HAS NO APPARENT SIGNATURE EXCEPT FOR A SLIGHT INFLECTION ALONG THE ITCZ AXIS. CONVECTION IS RELATED TO THE ITCZ. TROPICAL WAVE ALONG 136W S OF 16N MOVING W 15 KT. THE WAVE HAS BEEN ANALYZED SLIGHTLY FARTHER W BASED ON AN IMPROVING LOW-LEVEL CURVATURE TO THE WIND FIELD...AND CLOSER TO A CLUSTER OF SCATTERED MODERATE CONVECTION FROM 8N-14N BETWEEN 132W-140W. ...ITCZ... ITCZ AXIS IS CENTERED ALONG 7N77W 9N85W 8N95W 10N110W 12N133W 9N140W. NUMEROUS MODERATE/STRONG CONVECTION FROM 3N-8N E OF 81W. SCATTERED MODERATE FROM 5N-10N BETWEEN 83W-86W. SCATTERED MODERATE FROM 9N-14N BETWEEN 93W-97W. WIDELY SCATTERED MODERATE WITHIN 120 NM OF THE AXIS BETWEEN 93W-113W AND 116W-129W. SCATTERED MODERATE FROM 8N-14N W OF 132W. ...DISCUSSION... AN UPPER LEVEL ANTICYCLONE IS CENTERED OVER THE FAR NW PORTION OF THE AREA NEAR 28N138W WITH MODERATE/STRONG SUBSIDENCE EXTENDING NW OF A LINE FROM 30N122W TO 17N140W. A CLOSED UPPER LOW (AN OPEN TROUGH IN THE MID-LEVELS) LIES ADJACENT TO THE RIDGE/ANTICYCLONE CENTERED IN THE VICINITY OF 19N128W WITH UPPER MOISTURE WRAPPING PRIMARILY AROUND THE S AND E SIDES. WATER VAPOR IMAGERY INDICATES A SECOND UPPER LOW/TROUGH LOCATED OVER NRN BAJA CALIFORNIA AND IS REALLY ONLY SERVING TO ENHANCE THE SUMMER MONSOON RAINS OVER NW MEXICO AND THE SW UNITED STATES. ONE LINE OF TSTMS CURRENTLY EXTENDS ALONG THE COAST OF MEXICO FROM THE ISLAS MARIAS NW TO NEAR LOS MOCHIS...PROBABLY ALONG THE LAND BREEZE FRONT. ELSEWHERE...AN UPPER LEVEL ANTICYCLONE IS CENTERED FARTHER S NEAR 19N117W WITH DEEP TROPICAL EASTERLIES EXTENDING S OF 15N FROM CENTRAL AMERICA WWD TO 125W. STRONG UPPER LEVEL DIVERGENCE IS OCCURRING OVER THE ITCZ W OF 125W... AND IS ENHANCING CONVECTION ASSOCIATED WITH THE TROPICAL WAVE ALONG 136W. LOW-LEVEL CROSS-EQUATORIAL FLOW E OF 100W IS RATHER STRONG AT THE MOMENT WITH LOW CLOUD STREAMERS FLOWING INTO THE ITCZ FROM THE S. A TROPICAL SQUALL LINE CURRENTLY EXTENDS S OF THE GULF OF TEHUANTEPEC FROM 14N96W TO 10N95W MOVING W ABOUT 30 KT BUT THE TSTM ACTIVITY IS ON A DOWNWARD TREND. $$ BERG