GIFS-TIGGE WG 11th meeting, Exeter, UK Current Status and Plans of Ensemble Prediction System at KMA Seung-Woo Lee Numerical Model Development Division Korea Meteorological Administration.

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Transcript GIFS-TIGGE WG 11th meeting, Exeter, UK Current Status and Plans of Ensemble Prediction System at KMA Seung-Woo Lee Numerical Model Development Division Korea Meteorological Administration.

GIFS-TIGGE WG 11th meeting, Exeter, UK
Current Status and Plans of
Ensemble Prediction System
at KMA
Seung-Woo Lee
Numerical Model Development Division
Korea Meteorological Administration
Contents
• Outline of KMA operational EPS (KMA EPSG)
• Sensitivity test of KMA Hybrid Ensemble-4dVAR
• Future plans of KMA EPSs
• Summary
2
Brief history of KMA EPSG for TIGGE
2006.07.~2010.12.
2010.12~2011.05
2011.5~2012.6.
2012.6~2013.6
2013.7.~
Model Base
GDAPS (JMA)
UM (UKMO, ver7.5) UM ver7.7
UM ver7.9
UM ver7.9
Assimilation
Method
3D‐Var
4D‐Var
4D-Var
Hybrid Ensemble
4D‐Var
Horizontal
Resolution
N320 (~40km)
N320 (~40km)
T213 (Gausian grid)
0.5625 in lon/ 0.375 0.5625 in lon/
0.5625 degree in lat/lon
in lat.
0.375 in lat.
N320 (~40km)
0.5625 in lon/
0.375 in lat.
N320 (~40km)
0.5625 in lon/
0.375 in lat.
4D‐Var
Vertical levels / top
40 / ~0.4 hPa
of model
50 / ~63 km
70 / ~80 km
70 / ~80 km
70 / ~80 km
Initial
Times
00,12
00, 12
00,12
00,12
00, 12 (06, 18 for
cycled hybrid)
Lead
Time
10 days
10 days
10 days
10 days
12 days
Output
Frequency
6h
6h
6h
6h
6h to 240h,12h to
288
No. of
15+1
Members (+control)
23+1
23+1
23+1
23+1
Coupled
Ocean
No
No
No
No
No
Initial
Perturbations
Breeding + factor
rotation
ETKF
ETKF
ETKF
ETKF
Model
Perturbations
No
RP, SKEB2
RP, SKEB2
RP, SKEB2
RP, SKEB2
Surface
3 Perturbations
No
No
No
SST Perturbation SST Perturbation
Major change in EPSG in 2012~13
GDPS(N512L70)
OPS, VAR, UM
SST
statistics
4
Trim obstore
N512L70 T+0
Trimmed obstore
Initial Dump
Reconfiguration
OPS
N320L70 T+0
2012. 6.
Varobs
obstore
Varobs,modelobs
OPS background
-6 hour
EPSG cycle
FieldCalc
ETKF
ETKF background
Perts(SST)
VarSCR_UMFileUnit
Perts(u,v,p,q,t)
Perts(u,v,p,q,t,SST)
UM
N320L70
GDPS(N512L70)
4DVAR
+6 hour
EPSG cycle
OPS background
ETKF background
VAR background
2013. 7.
Sensitivity to ensemble members
5
OPER
M22
M44
Observations
KMA ODB
KMA ODB
KMA ODB
Data assimilation
4dVar
Hybrid Ens.
4dVar
Hybrid Ens.
4dVar
Ensemble members
excluding control
23
22
44
Model version
UM 7.9
UM 7.9
UM 7.9
Background error
Statistical BE
0.8*Statistical_BE
+ 0.5*Ens_BE
0.8*Statistical_BE
+ 0.5*Ens_BE
6
• Test period : 2012. 8. 3. 12Z -2012. 8. 3. 29. 12Z
2012083000
2012082900
2012082800
2012082700
6
2012082600
Stable after 36 hours
2012082500
8
2012082400
2012082300
2012082200
2012082100
2012082000
2012081900
2012081800
2012081700
2012081600
2012081500
2012081400
2012081300
2012081200
2012081100
2012081000
2012080900
2012080800
2012080700
2012080600
2012080500
2012080400
7
2012080300
2012080200
theta
Sensitivity to ensemble members
RMS averaged for all perturbation members and levels
Avg RMS of Perturbations
Unstable in model dynamics
due to gravity wave drag
parameterization.
5
4
t_oper
3
t_m22
2
t_m44
1
0
Sensitivity to ensemble members
NH Z500 error against with observation
• Spread increased significantly in NH and Tropics,
while the CRPSS and BSS are not significantly
changed.
7
Sensitivity to ensemble members
SH Z500 error against observation
• Spread decreased significantly only in SH.
• M44 is a little better than M22 until T+144
• Only Spread of both M22 and M44 is significant
at the critical level=0.05
8
Impact on typhoon 4-day forecast (GDPS)
OPER
Analysis
9
M22
M44
Considerations for implementation
RUN TIME (minute)
Operation
M22
M44
Trim
3
3
3
OPS
6
6
10
ETKF
5
5
10
Reconfiguration
2
2
2
SST
1
1
1
Forecast (10d/9h)
70
70/6
70/6
Data size: operation(2 times/day), M22/44(4 times/day)x ERLY/LATE
10
Operation
M22
M44
Trim
200M
200M
200M
OPS
6G
6G
12G
ETKF+SST
20G
20G
36G
Reconfiguration
3.5G
3.5G
3.5G
UM Forecast(10d/9h)
124G
131G/46G
265G/90G
TOTAL(1day)
308G
776G
1,484G
Sensitivity to cycle strategy
Type 1
06 UTC
GDAPS
ERLY
LATE
EPSG
ERLY
LATE
Type 2
GDAPS
EPSG
11
06 UTC
ERLY
LATE
LATE
12 UTC
ERLY
ERLY
(10d)
LATE
ERLY
LATE
LATE
ERLY
LATE
12 UTC
ERLY
ERLY
(10d)
18 UTC
LATE
LATE
18 UTC
ERLY
LATE
LATE
00 UTC
ERLY
ERLY
(10d)
LATE
GDAPS
LATE
EPSG
00 UTC
ERLY
ERLY
(10d)
Type 3
Type 4
06 UTC
ERLY
LATE
LATE
06 UTC
LATE
GDAPS
ERLY
LATE
EPSF
ERLY
LATE
12 UTC
ERLY
ERLY
(10d)
LATE
ERLY
(10d)
ERLY
LATE
12 UTC
ERLY
18 UTC
LATE
LATE
LATE
18 UTC
ERLY
ERLY
LATE
00 UTC
ERLY
ERLY
(10d)
LATE
LATE
00 UTC
ERLY
ERLY
(10d)
LATE
Number of ingested observations
• Period: 2012. 6. 26. 00 ~ 2012. 7. 11. 18 UTC
• About 85~90% of satellite data are ingested in
the early cycle experiments.
12
RMSE and Spread
Difference between each variant and 1st variant (Type 1)
13
Relative performances
1
4
3
3
3
3
2
4
1
4
3
1
4
4
3
3
2
4
1
3
3
4
3
4
• Independent early cycle (Type 3 and 4) showed
improved ensemble spread.
• Type 1 for NH, Type 4 for SH, and Type 1 or 3 for
Tropics
• Type 2 reveals poorer performance than other types
of hybrid
14
Verification against with observation
average of the difference ratio against the best for t850
average of the difference ratio against the best for Z500
5
8
7
4
6
3
Type 1
1안
4
Type 2
2안
3
ratio
ratio
5
Type
1안 1
Type
2안 2
2
Type
3안 3
Type 3
3안
2
Type 4
4안
Type
4안 4
1
1
0
0
RMSE RMSE RMSE RMSE SPREADSPREADSPREAD SPREAD
RMSE RMSE RMSE RMSE SPREADSPREADSPREAD SPREAD
NH
SH
TR
AR
NH
SH
TR
AR
NH
SH
TR
AR
NH
SH
TR
AR
3/1
4
2
1
3
3
2
4
3
1/4
3
1
3
3
2
4
• Hybrid implementation of type 3 showed improved ensemble spread for Northern and
Southern Hemisphere.
• Over the tropics and Asian region, type 2 and 4 showed improved performances.
15
Future plans of KMA EPSs
 Seamless prediction from medium range to sub seasonal scale
• Increased spatial resolution and ensemble members EPSG, which
covers forecast range of medium to sub-seasonal scale of 3~4-weeks.
 Coupling of ocean model
• Implementation of extended EPSG with coupled ocean model (Operation
planned in 2014)
- Plans to evolve EPSG covers one-month period of forecast.
 Convective scale ensemble prediction system
• Developing a convective scale EPS to provide short-range probabilities of
high impact weather over local area (Operation planned in 2015)
 Data Assimilation
• Further optimization of Hybrid Ensemble 4DVAR system (in 2013)
• Introducing of 4D Ensemble-Var (next generation EPSG, in 5 years)
- Aiming at direct ensemble data assimilation with 4dVar
16
Summary
• KMA has been operating and developing a global EPS.
− introducing SST perturbation, hybrid ensemble 4dVar.
− sensitivity test shows a minor improvement in 44-members of hybrid
ensemble 4dVar, and a similar effect for each configuration of
operating strategies.
• KMA has plan to operate a global high-resolution EPSG, which has
forecast lead times from medium-range up to 3-weeks in 2016.
− with the coupling of ocean model and aim at development of one
month forecast EPSG.
• Research and development for the convective scale ensemble
prediction system are conducted.
− targeting short-range probabilistic forecast of local high impact
weather.
17