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

 223 
 WTNT44 KNHC 112049
 TCDAT4
 TROPICAL STORM IRENE DISCUSSION NUMBER  29
 NWS TPC/NATIONAL HURRICANE CENTER MIAMI FL
 5 PM EDT THU AUG 11 2005
  
 THE OVERALL CONVECTIVE PATTERN OF IRENE HAS CHANGED LITTLE TODAY.
 THE SYSTEM IS ELONGATED WEST-NORTHWEST TO EAST-SOUTHEAST AND THE
 BEST ESTIMATE OF THE SURFACE CENTER LOCATION...BASED ON CURVED
 LOW-LEVEL CLOUD LINES AND CONTINUITY...IS NEAR THE WESTERN EDGE OF
 THE CLOUD SHIELD AND NOT FARTHER EAST INTO THE DEEP CONVECTION.
 SATELLITE INTENSITY ESTIMATES ARE 35 KT...45 KT...AND 55 KT FROM
 TAFB...SAB...AND AFWA...RESPECTIVELY. THE INITIAL INTENSITY IS
 BEING MAINTAINED AT 45 KT FOR THIS ADVISORY...BUT IT COULD BE A
 LITTLE HIGHER.
  
 THE INITIAL MOTION ESTIMATE IS 300/13...BASED MAINLY ON CONTINUITY
 AND AND PARTLY ON THE MODELS INDICATING A GRADUAL DECREASE IN
 FORWARD SPEED. THERE HAS NOT BEEN MUCH CHANGE IN THE MODEL FORECAST
 TRACKS OR THE MODELS' HANDLING OF THE SUBTROPICAL RIDGE TO THE
 NORTH OF IRENE AND THE ALLEGED WEAKENING OF THE WESTERN PORTION OF
 THE RIDGE AFTER 72 HOURS. HOWEVER...IT SHOULD BE NOTED THAT NONE OF
 THE MODELS CREATE A WEAKNESS IN THE RIDGE DUE TO A SHORTWAVE TROUGH
 MOVING INTO THE MEAN RIDGE POSITION. THE NOGAPS AND UKMET MODELS
 ERODE THE RIDGE AS A RESULT OF AMPLIFYING IRENE TO A SIZE NEARLY
 THE SAME AS THAT OF THE SYNOPTIC SCALE HIGH PRESSURE CENTER NEAR
 BERMUDA...WHICH RESULTS IN IRENE TURNING SHARPLY NORTHWARD ALONG
 70W LONGITUDE BY 72 HOURS. THAT SCENARIO SEEMS LESS LIKELY...GIVEN
 THE CURRENT SIZE AND STRENGTH OF THE BERMUDA RIDGE AS NOTED IN
 WATER VAPOR IMAGERY AND UPPER-AIR DATA. THE GFS HAS CONTINUED ITS
 TREND OF DISSIPATING IRENE WITHIN 48 HOURS AND MAINTAINING AN EAST-
 WEST ORIENTED MID-LEVEL RIDGE FROM BERMUDA WESTWARD TO THE
 CAROLINAS. THE OFFICIAL FORECAST IS CLOSE TO THE GFDL AND GFDN
 SOLUTIONS...WHICH MOVE IRENE FARTHER WEST AND CLOSER TO THE OUTER
 BANKS OF NORTH CAROLINA...AND DECREASE THE FORWARD SPEED TO ONLY 5
 KT AFTER 72 HOURS. THE OFFICIAL FORECAST IS NEARLY IDENTICAL TO THE
 PREVIOUS TRACK AND REMAINS NEAR THE LEFT EDGE OF THE MODEL GUIDANCE
 ENVELOPE. IT SHOULD BE POINTED OUT THAT WEAK STEERING CURRENTS LESS
 THAN 10 KT OFTENTIMES RESULTS IN ERRATIC MOTION...SO A POSSIBLE
 U.S. LANDFALL BY DAY 5 CAN NOT BE RULED OUT AT THIS TIME.
 
 AN UPPER-LOW TO THE SOUTH OF IRENE HAS BEEN ADVECTING DRY MID-LEVEL
 INTO THE SOUTHERN PORTION OF THE CYCLONE TODAY...WHICH HAS CAUSED
 THE CONVECTION TO ERODE AND WEAKEN AT TIMES. HOWEVER...WATER VAPOR
 IMAGERY INDICATES THE LOW HAS BEEN WEAKENING AND THAT THE MID- TO
 UPPER-LEVEL FLOW IS GRADUALLY BECOMING SOUTHEASTERLY. THEREFORE...
 DEEP CONVECTION HAS A BETTER CHANCE OF DEVELOPING LATER TONIGHT AND
 IRENE COULD BECOME A HURRICANE BY THIS TIME TOMORROW. LATER IN THE
 FORECAST PERIOD...DRY MID-LEVEL AIR REMAINS THE PRIMARY INHIBITING
 FACTOR. THE SHIPS MODEL HAS NOW DECREASED THE PEAK INTENSITY TO
 LESS THAN 70 KT DUE TO STRONG LOW-LEVEL ANTICYCLONIC FLOW
 SURROUNDING THE CYCLONE AS IT MOVES INTO A STRONGER RIDGE. THE
 OFFICIAL INTENSITY FORECAST REMAINS ABOVE THE SHIPS MODEL SINCE THE
 GFS-BASED SHIPS MODEL DOES NOT HOLD ONTO IRENE AFTER 48 HOURS...
 WHICH RESULTS IN AN ARTIFICIALLY STRONGER RIDGE IN THE GFS MODEL.
 
 FORECASTER STEWART
 
 FORECAST POSITIONS AND MAX WINDS
  
 INITIAL      11/2100Z 25.7N  63.9W    45 KT
  12HR VT     12/0600Z 26.7N  65.6W    55 KT
  24HR VT     12/1800Z 27.8N  67.6W    60 KT
  36HR VT     13/0600Z 28.5N  69.1W    65 KT
  48HR VT     13/1800Z 29.1N  70.5W    70 KT
  72HR VT     14/1800Z 31.0N  72.5W    75 KT
  96HR VT     15/1800Z 33.0N  73.5W    75 KT
 120HR VT     16/1800Z 35.0N  74.5W    75 KT
  
 $$
 
Return to the Tropical Systems Page for IRENE

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