Image Department Meteorology
Meteorology_Home Weather_Server News/Seminars
People
Research
Academics Application Contact_Us

Hawaiian_Weather
US_Mainland_Weather
Tropical_Weather
Satellite_Imagery
Radar_Imagery
Marine
Numerical_Models
LAPS
Forecasts
Observations
Archive
Links Disclaimer
Space
SOEST_Home
University_of_Hawaii_Home

 203 
 WTNT45 KNHC 170239
 TCDAT5
 TROPICAL STORM OMAR DISCUSSION NUMBER  15
 NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL   AL152008
 1100 PM EDT THU OCT 16 2008
 
 OMAR HAS A RATHER NON-TROPICAL APPEARANCE THIS EVENING...WITH LITTLE
 ORGANIZED CONVECTION NEAR THE CENTER.  RECENT AMSU MICROWAVE DATA
 INDICATES THAT OMAR HAS LOST ITS UPPER-LEVEL WARM CORE DUE TO
 SHEAR...BUT RETAINS A LOW/MID-LEVEL WARM CORE.  THAT...COMBINED
 WITH NO OBVIOUS EVIDENCE OF A LOW-LEVEL/SURFACE FRONTAL SYSTEM
 NEARBY...MEANS THAT IT REMAINS A TROPICAL CYCLONE DESPITE THE
 APPEARANCE.  A QUICKSCAT OVERPASS NEAR 22Z SHOWED A RELIABLE-LOOKING
 65 KT WIND VECTOR AND SEVERAL 60-KT VECTORS.  BASED ON THIS...OMAR
 IS BELIEVED TO HAVE BEEN A HURRICANE UP TO 00Z...BUT HAS NOW LIKELY
 WEAKENED TO A 60-KT TROPICAL STORM.
 
 THE INITIAL MOTION IS SLIGHTLY TO THE RIGHT OF THE PREVIOUS
 ADVISORY...040/22.  OTHER THAN THAT...THERE IS LITTLE CHANGE IN THE
 FORECAST PHILOSOPHY OR THE FORECAST TRACK.  OMAR IS MOVING
 NORTHEASTWARD BETWEEN A DEEP-LAYER TROUGH TO THE NORTHWEST AND A
 DEEP-LAYER RIDGE TO THE EAST.  THE TROUGH IS FORECAST TO LIFT OUT
 TO THE NORTHEAST...WHICH SHOULD CAUSE OMAR TO SLOW ITS FORWARD
 MOTION DURING THE NEXT COUPLE OF DAYS.  THE TRACK GUIDANCE IS
 TIGHTLY CLUSTERED AROUND A NORTH-NORTHEASTWARD MOTION THROUGH 72
 HR...AND THE NEW FORECAST TRACK IS JUST TO THE EAST OF THE MODEL
 CONSENSUS.  THERE IS SOME SPREAD IN THE LARGE-SCALE MODELS AFTER 72
 HR.  THE UKMET AND THE NOGAPS FORECAST OMAR TO TURN EASTWARD OVER
 THE TOP OF THE ATLANTIC RIDGE...WHILE THE GFS AND ECMWF FORECAST IT
 TO BE ABSORBED BY A STRONG NON-TROPICAL LOW MOVING EASTWARD ACROSS
 THE WESTERN ATLANTIC.  AT THIS TIME...IT IS UNCLEAR WHICH OF THESE
 SCENARIOS WILL BE CORRECT.  THUS...THE TRACK FORECAST CALLS FOR AN
 EASTWARD MOTION AT A SPEED BETWEEN THAT OF THE ABOVE MENTIONED
 GLOBAL MODELS.
 
 THE BIGGEST ISSUE ON THE INTENSITY FORECAST IS WHETHER OMAR WILL BE
 ABLE TO GENERATE ENOUGH CONVECTION TO CONTINUE TO BE CALLED A
 TROPICAL CYCLONE.  ANALYSES FROM CIMSS AT THE UNIVERSITY OF
 WISCONSIN SHOW THAT OMAR IS CURRENTLY UNDERGOING ABOUT 40 KT OF
 SOUTHWESTERLY VERTICAL WIND SHEAR.  THE LARGE-SCALE MODELS SUGGEST
 THAT THE CYCLONE WILL REMAIN IN AT LEAST MODERATE VERTICAL
 SHEAR...ALTHOUGH THERE IS THE POSSIBILITY THE SHEAR COULD DECREASE
 SOME IN THE NEXT 24 HR.  THE INTENSITY FORECAST FOR THE FIRST 48 HR
 FOLLOWS THE SCENARIO THAT OMAR WILL DEVELOP ENOUGH CONVECTION TO
 KEEP IF FROM DEGENERATING INTO A REMNANT LOW...BUT NOT ENOUGH TO
 KEEP IT FROM WEAKENING.  THUS...THIS PART OF THE FORECAST SHOWS
 GRADUAL WEAKENING.  AFTER 48 HR...OMAR WILL CROSS THE 26C SEA
 SURFACE TEMPERATURE ISOTHERM...ENCOUNTER INCREASING WIND SHEAR...
 AND BEGIN MERGING WITH A FRONTAL SYSTEM.  THE INTENSITY FORECAST
 CALLS FOR EXTRATROPICAL TRANSITION AT 72-96 HR...AND KEEPS OMAR AT
 35 KT DURING THIS TIME.  IF THE NOGAPS AND UKMET FORECASTS VERIFY...
 OMAR COULD RE-INTENSIFY AS AN EXTRATROPICAL LOW OVER THE EASTERN
 ATLANTIC.  HOWEVER...THAT IS TOO UNCERTAIN TO INCLUDE IN THE
 FORECAST AT THIS TIME.
  
 FORECAST POSITIONS AND MAX WINDS
  
 INITIAL      17/0300Z 23.8N  58.1W    60 KT
  12HR VT     17/1200Z 26.4N  56.2W    55 KT
  24HR VT     18/0000Z 29.3N  54.0W    50 KT
  36HR VT     18/1200Z 31.3N  51.9W    45 KT
  48HR VT     19/0000Z 33.3N  49.6W    40 KT
  72HR VT     20/0000Z 37.0N  43.5W    35 KT...BECOMING EXTRATROPICAL
  96HR VT     21/0000Z 38.0N  35.5W    35 KT...EXTRATROPICAL
 120HR VT     22/0000Z 38.0N  28.0W    35 KT...EXTRATROPICAL
  
 $$
 FORECASTER BEVEN
  
 
Return to the Tropical Systems Page for OMAR

Back to main Tropical Weather page




This page is maintained voluntarily by the MKWC and the UHMET faculty, staff, and students.
It was last modified on: Thu, Jul 23 2020 - 2003 UTC
Send comments to: Ryan Lyman