000 AXPZ20 KNHC 132138 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 2205 UTC MON AUG 13 2007 TROPICAL WEATHER DISCUSSION FOR THE EASTERN PACIFIC OCEAN FROM THE EQUATOR TO 32N...EAST OF 140W. BASED ON 1800 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH 2115 UTC. ...TROPICAL WAVES... TROPICAL WAVE HAS BEEN ADJUSTED ALONG 87W N OF 6N ESTIMATED TO BE MOVING W NEAR 15 KT. THIS ADJUSTMENT WAS BASED ON THE FORMATION OF A LOW PRES SYSTEM IN THE S CENTRAL GULF. FOR DETAILS REFER TO THE ATLANTIC TWD...MIATWDAT. IN THE EPAC...THERE IS ENHANCED TURNING BOTH TO THE E AND W OF THE ANALYZED AXIS...LIKELY ASSSOCIATED WITH ITCZ ENERGY. TROPICAL WAVE ALSO ADJUSTED ALONG 108W FROM 8N-17N MOVING W 10-15 KT. A 1010 MB LOW WAS ADDED TO THE WAVE AXIS ALONG 13N. VIS IMAGES SHOW AN ELONGATED AREA OF LOW PRES WITH LOW-LEVEL CENTER PARTIALLY EXPOSED TO THE E OF A CONVECTIVE BLOB FROM 13N-16N BETWEEN 109W-112W. TROPICAL WAVE IS ALONG 131W FROM 8N-15N MOVING W 10-15 KT. A 1011 MB WAS ADDED TO THE WAVE ALONG 13N. A FAIR AMOUNT OF LOW-LEVEL TURING IS EVIDENT ALONG THIS WAVE AXIS...ESPECIALLY NEAR THE WEAK LOW CENTER. THIS WAVE IS EMBEDDED IN A VERY STABLE ENVIRONMENT WHICH IS SUPPRESSING SIGNIFICANT SHOWER ACTIVITY. ...ITCZ... ITCZ AXIS IS ALONG 8N77W 13N90W 13N100W 15N105W 13N115W 14N130W 10N135W 10N140W. SCATTERED MODERATE CONVECTION FROM 3N TO 5N BETWEEN 80W AND 82W. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION FROM 8N TO 14N BETWEEN 93W AND 99W. SCATTERED MODERATE CONVECTION FROM 12N TO 15N BETWEEN 100W AND 104W. SCATTERED MODERATE TO ISOLATED STRONG CONVECTION FROM 12N TO 16N BETWEEN 108W AND 112W. SCATTERED MODERATE CONVECTION FROM 10N TO 12N BETWEEN 116W AND 121W. ...DISCUSSION... UPPER LEVEL TROUGHING EXTENDS ACROSS THE NW PORTION OF THE AREA ASSOCIATED WITH A LARGE ELONGATED UPPER LOW WELL N OF THE DISCUSSION AREA. UPPER LEVEL RIDGING HOLDS SE OF THERE WITH AN ANTICYCLONE CENTERED NEAR 21N115W AND NEAR 17N141W. A WEAK INVERTED TROUGH LIES BETWEEN THESE ANTICYCLONES. THIS OVERALL CONFLUENT PATTERN IS SUSTAINING WIDESPREAD DRY AIR ALOFT W OF 120W. THE TROPICAL ERN PACIFIC IS CONSIDERABLY MORE MOIST CONTRIBUTED TO A TROPICAL WAVES AND ITCZ DISTURBANCES. STRONG UPPER NELY FLOW...BETWEEN AN UPPER LOW IN THE GULF AND AN UPPER HIGH OVER MEXICO IS ALSO ADVECTING WIDESPREAD HIGH CLOUDINESS INTO THE REGION.THE STRONGEST CLUSTERS OF CONVECTION ARE EMBEDDED IN THE ITCZ...DISCUSSED ABOVE. AT THE SFC...RATHER WEAK RIDGING IS PRODUCING MODERATE WINDS ACROSS THE REGION. THIS PRES PATTERN MAY EVEN WEAKEN FURTHER OVER THE NEXT COUPLE OF DAYS SO EXTENSIVE AREAS OF STRONG WINDS (TRADES) ARE NOT ANTICIPATED AT THE MOMENT. ONE AREA TO WATCH IS AN AREA OF LOW PRES EXPECTED TO FORM IN THE GULF OF TEHUANEPEC IN THE NEXT DAY OR SO...HAVE WORKED SOME WINDS AROUND THIS LOW IN THE HIGH SEAS FORECAST. A BROKEN LAYER OF STRATOCUMULUS CLOUDS COVER MOST OF THE SUBTROPICS...INDICATING THE STABILITY IN THE REGION. $$ CANGIALOSI