| HOME | ARCHIVES | FORECASTS | IMAGERY | ABOUT NHC | RECONNAISSANCE |

Hurricane SEYMOUR (Text)


ZCZC MIATCDEP5 ALL
TTAA00 KNHC DDHHMM

HURRICANE SEYMOUR DISCUSSION NUMBER  14
NWS NATIONAL HURRICANE CENTER MIAMI FL       EP202016
800 AM PDT WED OCT 26 2016

Seymour continues to maintain an impressive central dense overcast,
consisting of very deep convection around a 15 n mi well-defined
eye.  However, the distribution of convection has become slightly
asymmetric since the last advisory, with the greatest coverage to
the north and east of the center.  The convective asymmetry is
likely indicative of some increase in southwesterly shear.  A blend
of the latest Dvorak T- and CI-numbers, including UW-CIMSS ADT
values, is used to lower the initial intensity estimate of 120 kt.

Seymour is living on borrowed time.  A large mid- to upper-level
trough seen in water vapor imagery upstream of the cyclone should
cause a considerable increase in southwesterly shear within 24
hours. By that time, Seymour will already have reached much cooler
waters.  This should result in weakening, with the rate of filling
only increasing with time.  By 36 hours, the shear should become
extremely strong and cause the vortex to shear apart, with the
middle and upper portions of the circulation moving well to the
north or northeast of the low-level center.  The official forecast
shows Seymour becoming a post-tropical remnant low in 48 hours in
general agreement with global models that depict this decoupling as
soon as 36 to 42 hours. The NHC intensity forecast shows about the
same rate of weakening as the previous one and is close to the
multi-model consensus.

The initial motion estimate is 290/13.  Seymour has begun to gain a
little more latitude recently as it nears the western periphery of a
mid-level ridge west of the Baja California peninsula.  The
cyclone's motion should slow and become northwesterly soon and
then shift north-northwestward and northward in 24 to 36 hours as
Seymour becomes embedded in the flow between the high to the
northeast and the trough to the northwest.  Once Seymour becomes a
shallow system in 48 hours, the remnant low will slow further and
turn north-northeastward until dissipation.  The NHC track forecast
is only slightly to the left of the previous one after 24 hours and
a little faster during the remnant low phase.


FORECAST POSITIONS AND MAX WINDS

INIT  26/1500Z 16.9N 120.2W  120 KT 140 MPH
 12H  27/0000Z 18.0N 121.5W  105 KT 120 MPH
 24H  27/1200Z 19.7N 122.6W   80 KT  90 MPH
 36H  28/0000Z 21.1N 122.9W   60 KT  70 MPH
 48H  28/1200Z 22.2N 122.4W   35 KT  40 MPH...POST-TROP/REMNT LOW
 72H  29/1200Z 23.7N 121.7W   25 KT  30 MPH...POST-TROP/REMNT LOW
 96H  30/1200Z...DISSIPATED

$$
Forecaster Kimberlain

NNNN

Standard version of this page

Alternate Formats
About Alternates - E-Mail Advisories - RSS Feeds

Cyclone Forecasts
Latest Advisory - Past Advisories - About Advisories

Marine Forecasts
Latest Products - About Marine Products

Tools & Data
Satellite Imagery - US Weather Radar - Aircraft Recon - Local Data Archive - Forecast Verification - Deadliest/Costliest/Most Intense

Learn About Hurricanes
Storm Names Wind Scale - Prepare - Climatology - NHC Glossary - NHC Acronyms - Frequently Asked Questions - AOML Hurricane-Research Division

About Us
About NHC - Mission/Vision - Other NCEP Centers - NHC Staff - Visitor Information - NHC Library

Contact Us


NOAA/ National Weather Service
National Centers for Environmental Prediction
National Hurricane Center
11691 SW 17th Street
Miami, Florida, 33165-2149 USA
nhcwebmaster@noaa.gov
Disclaimer
Privacy Policy
Credits
About Us
Glossary
Career Opportunities
Page last modified: Saturday, 31-Dec-2016 12:10:50 UTC