000 AXPZ20 KNHC 210324 TWDEP TROPICAL WEATHER DISCUSSION NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL 0405 UTC THU FEB 21 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... ITCZ AXIS IS CENTERED ALONG 5N77W 7N87W 4N104W 5N140W. SCATTERED SHOWERS/ISOLATED TSTMS FROM 3N-9N BETWEEN 84W-88W. SCATTERED MODERATE CONVECTION WITHIN 60 NM OF AXIS BETWEEN 116W-121W. ...DISCUSSION... SUBTROPICS... THE MID/UPPER LEVEL PATTERN ACROSS THE N PACIFIC WATERS AND NORTH AMERICA CONSISTS OF A GENERAL LARGE-SCALE RIDGE ALONG THE W COAST OF UNITED STATES AND A BROAD LONGWAVE TROUGH E OF THE ROCKY MOUNTAINS. BECAUSE OF THE PACIFIC RIDGE...A SPLIT FLOW REGIME IS IN PLACE BETWEEN HAWAII AND CALIFORNIA AS PART OF THE FLOW TURNS N TOWARDS ALASKA TO CIRCUMVENT THE RIDGE AND THE OTHER PART TURNS SE TOWARDS BAJA CALIFORNIA. A SHORTWAVE TROUGH IS MOVING EWD WITHIN THIS SOUTHERN PORTION OF THE SPLIT... EXTENDING FROM ARIZONA SW TO 20N126W AND CONNECTED TO A CUT-OFF LOW CENTERED OVER NW ARIZONA/SW UTAH. A DECAYING FRONTAL BOUNDARY ASSOCIATED WITH THE TROUGH IS DRAPED FROM SOUTHERN CALIFORNIA TO 27N123W TO 30N130W BUT NOW IS ONLY ASSOCIATED WITH A BROKEN DECK OF LOW/MID LEVEL CLOUDS. ANOTHER FRONT IS LOCATED JUST NW OF THE REGION AND IS EXPECTED TO EASE SE OF 30N140W BY THU AFTERNOON. THERE IS ENOUGH MOISTURE AHEAD OF THE FRONT THAT SCATTERED SHOWERS/ISOLATED TSTMS COULD DEVELOP PRIMARILY N OF 25N W OF 130W THROUGH THE DAY ON THU. HIGH PRES COVERS THE REMAINDER OF THE SUBTROPICAL WATERS WITH A 1022 MB HIGH CENTERED NEAR 25N126W. OVER MEXICO...THE SUBTROPICAL JET EXTENDS ACROSS BAJA CALIFORNIA TOWARDS W TEXAS WITH MAXIMUM WINDS OF 90 KT...AND A BROAD CANOPY OF CIRRUS EXTENDING 600 NM SE OF A LINE FROM 20N123W TO 31N109W. TROPICS... A LARGE CUT-OFF MID/UPPER LOW IS LOCATED DEEP IN THE TROPICS NEAR 10N139W AND IS EXPECTED TO REMAIN DETACHED FROM THE MID-LATITUDE FLOW FOR SEVERAL DAYS. AN 80 KT JET STREAK LIES ON THE SE PERIPHERY OF THE LOW BUT THE FEATURE IS NOT CAUSING ANY NOTICEABLE WEATHER. THE ITCZ IS QUITE LINEAR W OF 110W WITH ONLY SCATTERED SHOWERS/TSTMS WITHIN 60 NM OF ITS AXIS. FARTHER E...AN ELONGATED MID-LEVEL RIDGE AXIS EXTENDS FROM THE NW CARIBBEAN TO NEAR 13N120W AND IS CAUSING MODERATE SUBSIDENCE ACROSS SOUTHERN MEXICO. OTHERWISE...A FAIRLY PRONOUNCED UPPER LEVEL EASTERLY JET EMANATING FROM COLOMBIA IS ADVECTING HIGH LEVEL MOISTURE WESTWARD TO NEAR 100W. THIS HAS DEEPENED THE MOISTURE AVAILABILITY AND PRODUCED WIDESPREAD CLOUDINESS E OF 92W WITH ISOLATED EMBEDDED CELLS OF MODERATE CONVECTION PRIMARILY ALONG THE ITCZ. SCATTERED TSTMS HAVE ALSO DEVELOPED OVER THE MOUNTAINS OF SW GUATEMALA AND ARE CURRENTLY IN A DECAYING STAGE. $$ BERG