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Transcript of Improvements in Deterministic and Probabilistic Tropical Cyclone Surface Wind Predictions Joint...
![Page 1: Improvements in Deterministic and Probabilistic Tropical Cyclone Surface Wind Predictions Joint Hurricane Testbed Project Status Report Mark DeMaria NOAA/NESDIS/ORA,](https://reader035.fdocuments.in/reader035/viewer/2022062314/56649ea35503460f94ba6d29/html5/thumbnails/1.jpg)
Improvements in Deterministic and Probabilistic
Tropical Cyclone Surface Wind Predictions
Joint Hurricane Testbed Project Status Report
Mark DeMariaNOAA/NESDIS/ORA, Fort Collins, CO
John A. Knaff, Jack Dostalek and Kimberly J. Mueller
CSU/CIRA, Fort Collins, CO
Collaborators: Jim Gross (TPC), Charles Anderson (CSU),Buck Sampson (NRL),Miles Lawrence(TPC), Chris Sisko (TPC)
Presented at The Inter-Departmental Hurricane ConferenceMarch 3, 2004 Charleston, SC
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OUTLINE• Deterministic Intensity Forecast Improvements
– Can inner core data from aircraft and satellite improve SHIPS forecasts?
• Automated objective analysis and EOF analysis
– Compare neural network and linear regression models
• Probabilistic Surface Wind Forecast Improvements– Calculate operational track/intensity and wind radii-
CLIPER error distributions– Randomly sample errors using Monte Carlo method
• Generate probabilities of 34, 50, 64 and 100 kt winds
![Page 3: Improvements in Deterministic and Probabilistic Tropical Cyclone Surface Wind Predictions Joint Hurricane Testbed Project Status Report Mark DeMaria NOAA/NESDIS/ORA,](https://reader035.fdocuments.in/reader035/viewer/2022062314/56649ea35503460f94ba6d29/html5/thumbnails/3.jpg)
Decay-SHIPS and NHC Intensity Forecast Skill 2001-2003
-30
-25
-20
-15
-10
-5
0
5
10
15
20
12 24 36 48 60 72 84 96 108 120
Forecast Interval (hr)
Err
or
Rel
ativ
e to
SH
IFO
R (
%)
Decay SHIPS
NHC Official
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5 Basic Radial Profiles (Samsury and Rappaport 1991)
1
2
3
4
5
• Develop objective method for extracting similar information• Supplement with inner-core GOES data
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Variational Wind Analysis for Aircraft Data
• Combine 12 hours of recon data in storm-relative coordinates
• Perform automated quality control– Analyze data to determine if coverage is sufficient
• Designed to measure at least azimuthal wavenumber 0 and 1 – Compare data to “pre-analysis” to eliminate bad points
• Perform “variational” analysis to provide u,v on radial, azimuthal grid – azimuthal smoothing >> radial smoothing– Based on Thacker and Long (1988)
• Preliminary prediction based upon azimuthal average tangential wind
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AF Recon Flight Level Winds for Hurricane LiliEarth-Relative 10/02/02 0000-1200 UTC
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AF Recon Flight Level Winds for Hurricane LiliStorm-Relative 10/02/02 0000-1200 UTC
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Variational Wind Analysis for Lili10/02/02 0000-1200 UTC
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Isotachs (kt) from Variational Wind Analysis for Lili10/02/02 0000-1200 UTC
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Isotach Analyses for Hurricane Lili10/01 0000 UTC – 10/03 1200 UTC
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0
10
20
30
40
50
60
0 20 40 60 80 100
120
140
160
180
200
Radius (km)
Tan
gen
tial
Win
d (
m/s
)
10/01 00
10/01 12
10/02 00
10/02 12
10/03 00
10/03 12
Azimuthally Averaged Tangential Wind (r=0 to 200 km)Hurricane Lili 10/01 00 UTC to 10/03 12 UTC
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Comparison of Best Track and Variational Analysis Maximum Wind
(1995-2002 Cases)
y = 0.9743x - 0.1111
R2 = 0.903
0
20
40
60
80
100
120
140
160
180
0 20 40 60 80 100 120 140 160 180
Analysis Max Wind (kt)
Bes
t T
rack
Max
Win
d (
kt)
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EOF Analysis
• ~400 cases with recon and IR data (95-03)• 51 radial grid points, r = 4 km• How to relate 102 IR and wind values to intensity
change?– Empirical Orthogonal Function (EOF) Analysis
– Mathematical technique for extracting common patterns from datasets
– Apply to tangential wind and IR radial profiles
– Work with small set of patterns instead of the entire profiles
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Variance Explained by each EOF
0
10
20
30
40
50
60
70
80
90
1 6 11 16 21 26 31 36 41 46 51
Eigenvalue Number
Var
ian
ce E
xpla
ined
(%
)
Tangential Wind
IR Brightness TTang. Wind:99% w\ 6 EOF
IR Brightness T:99% w\ 4 EOF
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Tangential Wind and IR EOFs
-0.2
0
0.2
0.4
0.6
0.8
2 22 42 62 82 102 122 142 162 182 202
Radius (km)
No
rmal
ized
Val
ue
EOF 1
EOF 2
EOF 3
-0.4
-0.2
0
0.2
0.4
0.6
2 22 42 62 82 102 122 142 162 182 202
Radius (km)
No
rmal
ized
Val
ue
EOF 4
EOF 5
EOF 6
-0.4
-0.2
0
0.2
0.4
0.6
2 22 42 62 82 102 122 142 162 182 202
Radius (km)
No
rmal
ized
Val
ue
EOF 1
EOF 2
EOF 3
EOF 4
Tang. Wind 1-3
IR 1-4
Tang. Wind 4-6
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Part 1 Project Schedule
• Spring 2004: Develop statistical intensity model using EOF amplitudes – Provide adjusted SHIPS forecast based upon inner core
information
• Spring 2004: Compare neural network and regression techniques– Collaboration with Dr. Charles Anderson, CSU Computer Science
Department (Expert in Machine Learning Techniques)
• Summer 2004: Implement variational aircraft analysis at NHC/JHT
• Summer/Fall 2004: Test results on real-time forecasts
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Preliminary Neural Network ResultsDependent data test with 1989-2002 Sample
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Monte Carlo Model for Tropical Cyclone Surface Wind Probabilities
(Initial support from Insurance Friends of the National Hurricane Center)
• Calculate NHC track and intensity errors (along track and cross track) from multi-year sample
• Determine large set of tracks and intensities (realizations) centered around official forecast by randomly sampling from error distributions
• Estimate wind radii distributions from errors of radii-CLIPER model
• Calculate probabilities by number of times specified point comes with radii of specified wind speed relative to total number of realizations
• Run in real-time in 2003 season (starting August)
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Monte CarloWind ProbabilityModel
Example:
Hurricane Fabian
Aug 31 2003 18Z
Vmax=115 kt
R34 100 75 75 100R50 30 30 30 30R64 20 20 20 20
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Modifications based on 2003 Results
• Model Changes– Improved portable random number generator– Complete error field sampling (instead of 1-99th percentiles)– Modified for use in the Atlantic, East/Central Pacific, and western North
Pacific basins (i.e., Longitude … 0-360)– Option for 100 kt radii added for JTWC
• Error Components– Improved radii-CLIPER model
• Inclusion of initial wind radii asymmetries – radii match observed at t=0 hr
• R34 bias correction
– Intensity errors account forecast intensity and distance to land– Distributions being updated with 2003 cases
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Old New
Impact of Model Changes(Fabian 2003 Example)
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3.34
1.62
0.600.33
0.18
0.06
0.02
15.759.53
4.452.96 2.45
1.09
0.48
0.01
0.1
1
10
100
10 100 1000 10000 100000
Number of Realizations
Pro
ba
bil
ity
Err
or
(%) Average Maximum
Effect of Number of Realizations on Probability Estimate
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Sensitivity to the number of realizations
N=500 N=1000
N=2000 N=500000
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R34 R50
R64 R100
TyphoonMaemi
9/9/04 06 Z
Vmax=115 kt
R34 130 130 130 130R50 50 50 50 50R100 20 20 20 20
N=2000
![Page 25: Improvements in Deterministic and Probabilistic Tropical Cyclone Surface Wind Predictions Joint Hurricane Testbed Project Status Report Mark DeMaria NOAA/NESDIS/ORA,](https://reader035.fdocuments.in/reader035/viewer/2022062314/56649ea35503460f94ba6d29/html5/thumbnails/25.jpg)
Part 2 Project Schedule
• Spring 2004: Investigate variable grid options – Improve efficiency and for NDFD applications
• Spring 2004: Finalize probability model for 2004 season
• Summer/Fall 2004: Run at NHC in real-time for Atlantic and East Pacific cases
• Summer/Fall 2004: Coordinate with JTWC for real-time tests (directly on their ATCF)
• Winter 2004: Evaluate results from 2004 runs
• 2004 “Freebie”: Provide NHC and JTWC with updated Radii-CLIPER models