

by ims1.ust.hk (iPlanet Messaging Server 5.2 Patch 1 (built Aug 19 2002))
with ESMTPS id <[email-masked]> for alau@ims-ms-daemon
(ORCPT [email-masked]); Mon, 14 Feb 2005 17:50:13 +0800 (CST)
Received: from vacuum.cso.uiuc.edu (vacuum.cso.uiuc.edu [128.174.5.113])
by mx2.ust.hk (8.12.11/8.12.11) with ESMTP id j1E9o8P0045186	for
<[email-masked]>; Mon, 14 Feb 2005 17:50:09 +0800 (HKT)
Received: from vacuum.cso.uiuc.edu (vacuum.cso.uiuc.edu [128.174.5.113])
by vacuum.cso.uiuc.edu (8.12.11/8.12.11) with ESMTP id j1E8aqOV096974; Mon,
14 Feb 2005 03:43:20 -0600
Received: by LISTSERV.UIUC.EDU (LISTSERV-TCP/IP release 14.3)
with spool id          307783 for [email-masked]; Mon,
14 Feb 2005 03:43:19 -0600
Received: from delyte.lib.siu.edu (delyte.lib.siu.edu [131.230.73.222])
by          vacuum.cso.uiuc.edu (8.12.11/8.12.11) with ESMTP id j1E9hI64075286
for <[email-masked]>; Mon, 14 Feb 2005 03:43:18 -0600
Received: from delyte.lib.siu.edu (localhost [127.0.0.1])
by delyte.lib.siu.edu          (8.13.3/8.12.11) with ESMTP id j1E9h7eA012086
for          <[email-masked]>; Mon,
14 Feb 2005 03:43:11 -0600 (CST)
Received: (from ldm@localhost) by delyte.lib.siu.edu (8.13.3/8.12.11/Submit)
id          j1E9h7lS012085 for [email-masked]; Mon,
14 Feb 2005 03:43:07 -0600 (CST)
Date: Mon, 14 Feb 2005 03:43:07 -0600
From: SIU Weather Processor <[email-masked]>
Subject: Pacific-EN: Tropical Weather Discussion
Sender: WX-TROPL Tropical Storm and Hurricane WX products
<[email-masked]>
To: [email-masked]
Reply-to: [email-masked]
Message-id: <[email-masked]>
Precedence: list
X-LibAffairs-MailScanner: Found to be clean
X-MailScanner-From: [email-masked]
X-Perlmx-Spam: Gauge=XXXIIIIIIII, Probability=38%,
Report='HASHBUSTER_BLOCK_V2 3.4, LINES_OF_YELLING_3 0.671,
__HASHBUSTER_BLOCK_V2_1 0, __HAS_MSGID 0, __LINES_OF_YELLING 0, __SANE_MSGID 0'

AXPZ20 KNHC 140942
TWDEP

TROPICAL WEATHER DISCUSSION
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
1005 UTC MON FEB 14 2005

TROPICAL WEATHER DISCUSSION FOR EASTERN PACIFIC OCEAN FROM
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
0930 UTC.

..ITCZ...
INTERTROPICAL CONVERGENCE ZONE...1N79W 6N90W 5N110W 7N126W
6N140W. NO SIGNIFICANT CONVECTION.

DISCUSSION...
W OF 120W...
LARGE WELL DEFINED CYCLONIC CIRCULATION WELL N OF THE AREA
NEAR 36N133W APPEARS TO BE LIFTING NWD AT 10 KT. ASSOCIATED MID
TO UPPER LEVEL TROUGH EXTENDS INTO THE DISCUSSION AREA N OF
26N W OF 130W. TROUGH SUPPORTS A COLD FRONT EXTENDING FROM
30N130W TO 22N140W. BROAD AREA OF STRONG WSWLY FLOW AT THE UPPER
LEVELS COVERS THE REMAINDER OF THE AREA SE OF THE TROUGH. THE
FLOW IS SOMEWHAT DIFFLUENT S OF 23N. MODERATE TO STRONG SWLY
WINDS ARE ADVECTING MID AND UPPER LEVEL MOISTURE NEWD TOWARD
SOUTHERN CALIFORNIA.

100W TO 120W...
MID TO UPPER LEVEL ANTICYCLONE VIRTUALLY DOMINATES THE AREA
BETWEEN 100W AND 120W. STRONG UPPER LEVEL SUBSIDENCE/DRY AIR
ALOFT COVERS THE AREA FROM 10N TO 25N. A WEAK CYCLONIC
CIRCULATION NEAR 10N116W IS SLIDING ESE AT 10-15 KT BENEATH THE
ANTICYCLONE. SOME UPPER LEVEL MOISTURE IS BEING ADVECTED EWD
ACROSS EXTREME NORTHERN MEXICO ALONG THE PERIPHERY OF THE
ANTICYCLONE.

E OF 100W...
WEAK UPPER LEVEL CYCLONIC CIRCULATION NEAR 10N99W IS MOVING WWD
10 KT AND IS ENHANCING SOME ISOLATED MODERATE CONVECTION ALONG
THE ITCZ BETWEEN 90W AND 96W. THE REMAINDER OF THE AREA IS
DOMINATED BY MODERATE SWLY FLOW AND STRONG SUBSIDENCE/DRY AIR
ALOFT.

$$
COBB

+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+-+
To unsubscribe from WX-TROPL send e-mail to [email-masked] with
"unsub wx-tropl" in the body of your message. For help with WX-TROPL
write to [email-masked] or see http://wxlist.5280tech.com. For more
information on tropical weather products, see the NHC Homepage
at http://www.nhc.noaa.gov.