Skip Navigation Links weather.gov   
NOAA logo - Click to go to the NOAA homepage National Weather Service   NWS logo - Click to go to the NWS homepage
National Hurricane Center
Local forecast by
"City, St" or "ZIP"

 
Get Storm Info
   Satellite | Radar
   Aircraft Recon
   Advisory Archive
   Experimental
   Mobile Products
   E-mail Advisories
   Audio/Podcasts
   GIS Data | RSS XML/RSS logo
   Help with Advisories
Marine Forecasts
   Atlantic and E Pacific
   Analysis Tools
   Help with Marine
Hurricane Awareness
   Be Prepared | Learn
   Frequent Questions
   AOML Research
   Hurricane Hunters
   Saffir-Simpson Scale
   Forecasting Models
   Eyewall Wind Profiles
   Glossary/Acronyms
   Storm Names
   Breakpoints
Hurricane History
   Seasons Archive
   Forecast Accuracy
   Climatology
   Most Extreme
About the NHC
   Mission and Vision
   Personnel | Visitors
   NHC Virtual Tour
   Library
   Joint Hurr Testbed
   The NCEP Centers
Contact UsHelp
FirstGov.gov is the U.S. Government's official Web portal to all Federal, state and local government Web resources and services.

Tropical Storm ZETA


ZCZC MIATCDAT5 ALL
TTAA00 KNHC DDHHMM
TROPICAL STORM ZETA DISCUSSION NUMBER  10
NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
4 PM EST SUN JAN 01 2006
 
ALTHOUGH THE CONVECTION IS NOT VERY DEEP...ZETA'S CLOUD PATTERN HAS
BECOME MORE SYMMETRIC OVER THE PAST FEW HOURS.  THIS SUGGESTS THAT
THE VERTICAL SHEAR MAY HAVE...AT LEAST TEMPORARILY...RELAXED
SLIGHTLY.  DVORAK INTENSITY ESTIMATES FROM TAFB AND SAB...ALONG
WITH AMSU ESTIMATES FROM THE UNIVERSITY OF WISCONSIN CIMSS...
CONTINUE TO SUPPORT A CURRENT WIND SPEED OF 45 KT.  GLOBAL MODEL
GUIDANCE INDICATES THAT WESTERLY SHEAR SHOULD INCREASE SOON AND
THIS WILL LIKELY CAUSE WEAKENING.  THE SHIPS MODEL...USING THE GFS
OUTPUT...SHOWS VERTICAL SHEAR OF 50 KT ON ZETA WITHIN 12 HOURS. 
THIS IS LIKELY AN EXAGGERATION CAUSED BY AVERAGING OVER TOO LARGE
OF A HORIZONTAL AREA AROUND THE STORM AND...POSSIBLY...TOO DEEP OF
A VERTICAL LAYER.  THE SHIPS MODEL CALCULATES THE SHEAR FROM THE
850 TO THE 200 MB LEVEL.  PHASE SPACE ANALYSES FROM FLORIDA STATE
UNIVERSITY SHOW THAT ZETA HAS A RATHER SHALLOW WARM CORE SO IT MAY
NOT HAVE AS DEEP A VERTICAL EXTENT AS MOST TROPICAL CYCLONES...AND
IT MAY NOT BE AS RESPONSIVE TO SHEAR PRODUCED BY
UPPER-TROPOSPHERIC...I.E. NEAR 200 MB...WINDS AS A TYPICAL TROPICAL
STORM.  THE OFFICIAL FORECAST DOES NOT WEAKEN THE CYCLONE AS
RAPIDLY AS SHIPS.

ZETA HAS BEEN MEANDERING IN A PARTIAL COUNTERCLOCKWISE LOOP
TODAY...PERHAPS ASSOCIATED WITH A BROADER-SCALE MID-TROPOSPHERIC
CYCLONIC CIRCULATION.  ASSUMING THAT THE STORM WEAKENS AS
FORECAST...THE SYSTEM SHOULD BEGIN TO RESPOND MORE TO THE
EAST-NORTHEASTERLY FLOW ON THE SOUTH SIDE OF A WEAK AND NARROW LOW-
TO MID-LEVEL RIDGE.  THE CONSENSUS OF THE TRACK MODEL GUIDANCE GOES
ALONG WITH THAT IDEA...AS DOES THE OFFICIAL FORECAST.
 
FORECASTER PASCH
 
 
FORECAST POSITIONS AND MAX WINDS
 
INITIAL      01/2100Z 25.0N  38.2W    45 KT
 12HR VT     02/0600Z 24.7N  39.2W    40 KT
 24HR VT     02/1800Z 24.5N  40.3W    35 KT
 36HR VT     03/0600Z 24.4N  41.4W    30 KT
 48HR VT     03/1800Z 24.4N  42.4W    25 KT...REMNANT LOW
 72HR VT     04/1800Z...DISSIPATED
 
 
$$
NNNN


Quick Navigation Links:
NHC Active Storms  -  Atlantic and E Pacific Marine  -  Storm Archives
Hurricane Awareness  -  How to Prepare  -  About NHC  -  Contact Us

NOAA/ National Weather Service
National Centers for Environmental Prediction
National Hurricane Center
Tropical Prediction Center
11691 SW 17th Street
Miami, Florida 33165-2149 USA
nhcwebmaster@noaa.gov
Disclaimer
Credits
Information Quality
Glossary
Privacy Policy
Freedom of Information Act (FOIA)
About Us
Career Opportunities
Page last modified: Tuesday, 03-Jan-2006 16:54:16 GMT