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Date: Mon, 02 Feb 2004 15:48:25 -0600
From: SIU Weather Processor <[email-masked]>
Subject: Pacific-NC: Tropical Weather Discussion
Sender: WX-TROPL Tropical Storm and Hurricane WX products
<[email-masked]>
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X-Perlmx-Spam: Gauge=XXXIII, Probability=33%, Report='UPPERCASE_75_100 1.489,
HASHBUSTER_BLOCK_V2 1.454, LINES_OF_YELLING_3 0.671, LINES_OF_YELLING 0.001,
LINES_OF_YELLING_2 0.001, TO_BE_REMOVED_REPLY 0.000'

ACPA40 PHFO 022149
TWDPA

TROPICAL WEATHER DISCUSSION
NWS CENTRAL PACIFIC HURRICANE CENTER HONOLULU HI
2200 UTC FEBRUARY 2 2004

CENTRAL NORTH PACIFIC...FROM 30N TO EQUATOR BETWEEN 140W AND 180
CENTRAL SOUTH PACIFIC...FROM 25S TO EQUATOR BETWEEN 120W AND 180

BASED ON METEOROLOGICAL ANALYSIS THROUGH 1800 UTC AND SATELLITE
IMAGERY THROUGH 2100 UTC.  MOVEMENTS AND TRENDS PAST 24 HOURS UNLESS
STATED OTHERWISE.

CENTRAL NORTH PACIFIC

TROPICAL CYCLONES/DISTURBANCES...NONE.

OTHER SIGNIFICANT FEATURES...
ITCZ...ISOLATED CBS E OF 142W BETWEEN 11N AND 08N AND ALSO
W OF 176W BETWEEN 07N AND 05N BOTH MOVING W 5 KT.
LITTLE CHANGE IN INTENSITY.

FRONT/SHEAR LINE...OVERCAST LOW TO MIDDLE CLOUDS WITH EMBEDDED
SHOWERS WITHIN 30N173W 26N 180 MOVING E KTS.

UPPER LOW...NEAR 19N147W STATIONARY.

MAIN HAWAIIAN ISLANDS...KAUAI TO THE BIG ISLAND OF HAWAII...
NO SIGNIFICANT CONVECTION.  FOR DETAILS...SEE THE LATEST HAWAIIAN
ISLANDS SATELLITE INTERPRETATION MESSAGE WITH WMO HEADER ATHW40 PHFO
AND AWIPS HEADER HFOSIMHI.

NORTHWEST HAWAIIAN ISLANDS...KURE ATOLL TO NIHOA INCLUDING MIDWAY...
SEE OTHER SIGNIFICANT FEATURES...WITHIN ABOVE FRONTAL BAND.

JOHNSTON ISLAND...
NO SIGNIFICANT CONVECTION.

ELSEWHERE...
NO SIGNIFICANT CONVECTION.

CENTRAL SOUTH PACIFIC

TROPICAL CYCLONES/DISTURBANCES...NONE.

OTHER SIGNIFICANT FEATURES...
TROUGH 25S159W 20S159W 10S173W 09S180 STATIONARY.
OCCASIONAL CBS WITHIN 100NM OF LINE 25S157W 11S161W AND ALSO
WITHIN 150NM OF POINT 09S174W STATIONARY WITH LITTLE CHANGE IN
INTENSITY.

AMERICAN SAMOA AND THE INDEPENDENT STATE OF SAMOA...
NO SIGNIFICANT CONVECTION.

ELSEWHERE...
NO SIGNIFICANT CONVECTION.

$$

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