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Tropical Cyclone Weekly Summary #119 (November 7 - 14, 1993)

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JACK

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Nov 14, 1993, 8:28:00 PM11/14/93
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This report is compiled from warnings issued by:
National Hurricane Center Central Pacific Hurricane Center
Naval Western Oceanography Center Fiji Meteorological Service
Meteorological Service of New Zealand Joint Typhoon Warning Center
Japanese Meteorological Agency Bureau of Meteorology, Australia
Philippine Meteorological Service Royal Observatory of Hong Kong
Indian Meteorological Department Reunion Meteorological Service
Mauritius Meteorological Service
(others may be added as they become available)

Author's note: ja...@cloud3.met.fsu.edu is still valid, but please try to
address any comments or questions to be...@hrd-tardis.nhc.noaa.gov (assuming
the mailer stays operational!).

WEEKLY TROPICAL CYCLONE SUMMARY #119: NOVEMBER 7 - 14, 1993

North Atlantic Basin: No tropical cyclones.

Eastern North Pacific Basin (E of 140 Deg. W): No tropical cyclones.

Central North Pacific Basin (180 Deg. W to 140 Deg. W): No tropical cyclones.

Western North Pacific Basin (W of 180 Deg. W):

Tropical Storm Jeana: At the start of the summary period, Jeana was west of
Guam moving west with 45 kt winds. Jeana turned west-northwest on 8 November as
it weakened to minimal tropical storm strength, then it turned north the next
day as it re-intensified. Jeana moved northeast on 10 November as it reached a
peak intensity of 60 kt. An eastward turn occurred the next day as Jeana weak-
ened, and rapid weakening to depression status occured on 12 November. Jeana
dissipated as a tropical cyclone later on 12 November near 22N 141E, although
the remnant disturbance was trackable for 1 more day as it moved north. Jeana
passed over Guam early in it's life, but there are no reports of damage or
casualties at this time.

Tropical Depression: A tropical depression formed near 6N 145E on 14 Novem-
ber. At the end of the summary period, it was moving slowly west with 30 kt
winds.

North Indian Ocean Basin:

Tropical Depression: A tropical depression formed in the Arabian Sea be-
tween India and the Maldives Islands near 7N 77E on 8 November. Moving north-
northeast, the system moved inland over southern India the next day and dis-
sipated over land on 10 November. Maximum sustained winds in this system are
estimated at 25 kt. There are no reports of damage, casualties, or significant
weather at this time.

Tropical Cyclone 01A: As far as the author can tell, this system formed
from the same monsoon disturbance that spawned the tropical depression. A
tropical depression formed near 14N 68E on 12 November. Moving west-northwest,
the system reached tropical storm intensity later that day. TC-01A moved
northwest on 13 November as it reached hurricane intensity, then it recurved
north-northeast on 14 November. At the end of the summary period, TC-01A was
moving north-northeast toward Pakistan with 85 kt winds.

South Indian Ocean Basin (W of 135 Deg. E):

Tropical Cyclone Alexina (TC-01S): This system formed as a cyclone pair
with the systems in the North Indian Ocean. A tropical depression formed near
12S 80E on 9 November. Initially moving west-southwest, the system reached
tropical storm intensity later that day. Alexina moved slowly south-southwest
on 10 November as it reached a peak intensity of 65 kt. It then turned south-
east on 11 November and south-southeast on 12 November while weakening. Alexina
turned southwest on 13 November as it weakened to a depression, and the system
dissipated the next day near 15S 80E.

South Pacific Ocean Basin (E of 135 Deg. E): No tropical cyclones.

Disclaimer: While an effort has been made to make sure this information is
accurate as possible, it was drawn from operational warnings that may not
always agree with the best track information published after the storm is
over. Please address any questions or comments by e-mail to Jack Beven at
Internet address:

be...@hrd-tardis.nhc.noaa.gov (preferrable)

or

ja...@cloud3.met.fsu.edu (still good for now)

Past copies of the Tropical Cyclone Weekly Summary can be obtained via e-
mail. Please send an e-mail message if you are interested.

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