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Improvements in Deterministic and Probabilistic Tropical Cyclone Wind Predictions:
A Joint Hurricane Testbed Project Update
Mark DeMaria and Ray ZehrNOAA/NESDIS/ORA, Fort Collins, CO
John Knaff and Kimberly Mueller
CIRA/CSU, Fort Collins, CO
Presented at The Interdepartmental Hurricane ConferenceMarch 2005 Jacksonville, FL
Outline• Deterministic Intensity Prediction
– GOES and Recon Intensity Prediction (GRIP) model• Predictors from aircraft recon and IR radial structure
combined with SHIPS forecasts
– Evaluate neural network techniques
• Probabilistic Intensity Prediction – Monte Carlo wind probability model
• Results from 2004• 2005 Plans
• Are Intensity Forecasts Improving?
The 2004 SHIPS Model• Statistical-dynamical intensity model (12-120 hr)• Developed from 1982-2003 sample• Empirical decay for portion of track over land• Track from adjusted 6-hour old NHC forecast• Version with satellite input operational for 2004• SHIPS Input
– Climatological: Julian Day – Atmospheric Environment: Shear, T200, 200, 850 – Oceanic Environment: SST, Ocean Heat Content– Storm Properties: Vm, dVm/dt, motion, PSL, lat, GOES Cold Pixel
Count, GOES TB Std Dev • Most storm property inputs are indirect measurements
SHIPS Forecast Skill 2004 Atlantic Sample
-10
0
10
20
30
40
50
12 24 36 48 60 72 84 96 108 120
Forecast Interval (hr)
Err
or
Re
lati
ve
to
SH
IFO
R5
Operational
Modified Decay Model
Aircraft Data in the GRIP Model
• USAF Reserve and NOAA aircraft data– Highly utilized for intensity estimation– Under utilized for intensity prediction
• Real time automated analysis system– Real time aircraft database set up on NCEP IBM (C.
Sisko)– Move data to storm-relative coordinates– Automated quality control
• Test for data coverage• Gross error check• Check deviations from pre-analysis
– Variational objective analysis in cylindrical coordinates• Greater azimuthal than radial smoothing
Sample Analysis for Hurricane Jeanne 2004
Input Data Wind Analysis Isotachs
358 Dependent Cases (1995-2003, 12 hour intervals)124 Independent Cases (2004, 6 hour intervals)Input to GRIP Model: Azimuthally Averaged Tangential Wind
GOES Data in the GRIP Model
• SHIPS already includes cold pixel count and Tb standard deviation (area averages)
• Examine radial structure of GOES data for predictive signal
-100
-80
-60
-40
-20
0
20
0 100 200 300 400 500
Radius (km)
Bri
gh
tnes
s T
emp
erat
ure
(C
)
AzimuthalAverage
GRIP Model Statistical Development
• GRIP Predictors– EOF Version
• SHIPS Forecast• Amplitudes of first four EOFs of GOES and Recon profiles (principal
components)
– Physical Version• SHIPS Forecast• 10 physical parameters from GOES and recon profiles
• Final GRIP Model– EOF Version
• SHIPS forecast, 2 recon PCs, 1 GOES PC
– Physical Version• SHIPS forecast, 3 recon variables, 1 GOES variable
• Both versions tested on 124 cases from 2004 Atlantic season
GRIP Model Results2004 Independent Cases
-8
-6
-4
-2
0
2
4
6
12 24 36 48 60 72 84 96 108 120
Forecast Interval (hr)
Pe
rce
nt
Imp
rov
em
en
t
Physical Input
Principal Component Input
2005 GRIP Model
• Add 2004 cases and re-derive the coefficients– ~20% increase in sample size
• Consider combined EOF and physical variable version
• Run in real time during 2005 season for further evaluation
Neural Network Model(Short Version: It didn’t work)
• NN Model Development – SHIPS dependent dataset used for training
• Non-satellite version– Development by Prof. Chuck Anderson, CSU computer
science department– 5 to10% reduction in mean absolute error in dependent
sample (12-120 hr)• Independent tests
– 2-5% degradation – NN Method appears to over-fit training data– One final try with more stringent fitting requirements
• Restrict input to only those predictors selected by SHIPS
Monte Carlo Wind Probability Model
• Provides 5 day surface wind probabilities– 34, 50 and 64 kt
• Historical NHC track, intensity and radii-CLIPER error distributions– Includes forecast interval time continuity and bias
corrections
• Run in real time on NCEP IBM during 2004• Results displayed on password-protected CIRA
web site– Atlantic, east, central and western N. Pacific sectors
Sample 34 kt Wind Probabilities
2005 Monte Carlo Model
• Move web page to TPC w\ N-AWIPS graphics• Add t=0 hour probabilities• Include radii adjustment
– Convert max in quadrant to average in quadrant• Ratios based upon H*Wind analyses
• Provide TPC with distribution calculation code• Text product under development• Training being developed • Verification system still needed
– Verification system could be used for all TC probabilistic forecasts (ensemble based, etc)
Are Intensity Forecasts Improving?
• 20 Year Atlantic sample (1985-2004)
• Verification with consistent set of rules– All cases except extra tropical– Official, Persistence, SHIFOR, SHIPS and
GFDL
• Consider only 48 hour forecasts
48 Hour Intensity Errors1985-2004
0
5
10
15
20
25
30
35
19
85
19
86
19
87
19
88
19
89
19
90
19
91
19
92
19
93
19
94
19
95
19
96
19
97
19
98
19
99
20
00
20
01
20
02
20
03
20
04
Year
Fo
rec
as
t E
rro
r (k
t)
PersistenceSHIFOROFCLSHIPSGFDL
48 Hour Intensity Forecast ErrorsNormalized by Persistence Errors
-20
-10
0
10
20
30
40
50
1985
1986
1987
1988
1989
1990
1991
1992
1993
1994
1995
1996
1997
1998
1999
2000
2001
2002
2003
2004
Year
Imp
rov
em
en
t o
ve
r P
ers
iste
nc
e (
%)
OFCL
SHIPS
SHIFOR
Linear (OFCL)
Linear (SHIPS)
Linear (SHIFOR)
Summary• GRIP Model to be tested in real time during
2005 season– 2004 results are encouraging
• Last chance for neural network model
• Monte Carlo probability model development continuing in 2005
• Intensity forecasts are improving
Ref: Further improvements to SHIPS, Weather and Forecasting, in press.