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Tropical Weather Discussion
000
AXPZ20 KNHC 180951
TWDEP
TROPICAL WEATHER DISCUSSION
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
1005 UTC MON OCT 18 2004
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 0600 UTC SURFACE ANALYSIS AND SATELLITE IMAGERY THROUGH
0915 UTC.
...SPECIAL FEATURES...
1007 MB LOW CENTER NEAR 15.5N109W AT 0600 UTC MOV W 10 KT.
CHANNEL 2 INFRARED SATELLITE IMAGERY INDICATES THAT THE LOW
PRESSURE AREA MAY BE ELONGATED ALONG A SW-NE AXIS WITH ANOTHER
LOW LEVEL CENTER NEAR 15N110.7W...CLOSER TO A BURST OF SCATTERED
STRONG CONVECTION WHICH EXISTS FROM 14.5N TO 16.5N BETWEEN
111.5W AND 113W. EASTERLY SHEAR IS OCCURRING IN THE VICINITY OF
THE SYSTEM...THUS INHIBITING ANY DEVELOPMENT FOR NOW.
...TROPICAL WAVES...
TROPICAL WAVE N OF 7N ALONG 99W/100W MOVING W 10-15 KT. CYCLONIC
TURNING NOTED EARLIER ALONG THE ITCZ HAS WEAKENED. WIDELY
SCATTERED MODERATE CONVECTION ACCOMPANIES THE WAVE AT ITS
INTERSECTION WITH THE ITCZ.
...ITCZ...
INTERTROPICAL CONVERGENCE ZONE AXIS...8N83W 6N90W 10N105W 12N114W
8N127W 11N140W. WIDELY SCATTERED MODERATE ISOLATED STRONG WITHIN
150 NM EITHER SIDE OF AXIS BETWEEN 85W AND 100W...WITHIN 150 NM
S OF THE AXIS BETWEEN 107W AND 110W...AND WITHIN 150-180 NM N OF
THE AXIS W OF 138W.
...DISCUSSION...
W OF 120W...
RATHER COMPLEX PATTERN W OF 120W AT THIS TIME. AT THE MID AND
UPPER LEVELS A SHEARING TROUGH EXTENDS FROM 32N122W SOUTHWESTWARD
ALONG 25N135W TO AN MID LEVEL CYCLONE WELL W OF THE AREA NEAR
21N149W. STRONG MID LEVEL SUBSIDENCE NOTED WITHIN 90 NM EITHER
SIDE OF SHEAR AXIS W OF 132W. BROAD SWLY FLOW AT THE UPPER
LEVELS AND ASSOCIATED MOISTURE PLUME IS RIDING OVER THE MID
LEVEL SUBSIDENCE W OF 135W...THIS MOISTURE SPREADS
ANTICYCLONICALLY NE ACROSS THE NORTHERN BAJA PENINSULA AND SEA
OF CORTEZ...ACROSS NORTHERN OLD MEXICO AND TEXAS. SATELLITE
DERIVED WINDS INDICATED AN UPPER LEVEL WIND MAX OF 70-90 KT
ALONG 24N140W THROUGH 32N124W. AT THE SURFACE A FRONTAL TROUGH
EXTENDS FROM 30N127W TO 29N140W AND IS MOVING SE AT 10-15 KT.
E OF 120W...
UPPER LEVEL ANTICYCLONE CENTERED NEAR 21N109W DOMINATES THE FLOW
BETWEEN 100W AND 120W. ASSOCIATED RIDGE AXIS EXTENDS WESTWARD
FROM THE SOUTHERN GULF OF MEXICO NEAR 23N95W THROUGH 16N120W.
EASTERLY FLOW S OF THE ANTICYCLONE IS SHEARING CONVECTION WELL
AWAY FROM THE 1007 MB LOW NEAR 15.5N109W. A BAND OF MODERATE MID
TO UPPER LEVEL SUBSIDENCE COVERS THE AREA FROM 12N TO 25N
BETWEEN 90W AND 120W...WITH THE STRONGEST SUBSIDENCE NOTED OVER
THE YUCATAN PENINSULA/BAY OF CAMPECHE AND BUILDING TOWARD THE
GULF OF TEHUANTEPEC.
AN UPPER ANTICYCLONE SE OF AREA NEAR 12S87W HAS RIDGE AXIS NW
ACROSS THE EQUATOR TO 10N100W. ANOTHER UPPER ANTICYCLONE IS
NOTED NEAR 13N78W. RESULTANT UPPER DIFFLUENCE IS ENHANCING ITCZ
CONVECTION BETWEEN 85W AND 100W. MID LEVEL CYCLONIC TURNING WAS
NOTED ALONG THE ITCZ IN THE VICINITY OF 9N94W AND 8N87W.
$$
COBB
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