Upload
taite
View
39
Download
0
Embed Size (px)
DESCRIPTION
T argeted T raining A ctivity: S easonal P redictability in T ropical R egions: R esearch and A pplications. Seasonal Predictability in East Asian Region. - PowerPoint PPT Presentation
Citation preview
Seasonal Predictability Seasonal Predictability in East Asian Region in East Asian Region
TTargeted argeted TTraining raining AActivity:ctivity:
SSeasonal easonal PPredictability in redictability in TTropical ropical RRegions: egions: RResearch and esearch and AApplicationspplications
『 『 East Asian East Asian GroupGroup 』』
Juhyun Park (Republic of Juhyun Park (Republic of Korea)Korea)
Yanju Liu (China), qiaoping Yanju Liu (China), qiaoping
Li (China)Li (China) N. Jyothi (India), A. N. Jyothi (India), A. P. Dimri (India)P. Dimri (India)
Table of ContentsTable of Contents
3. Deterministic Forecast skill in DMME3. Deterministic Forecast skill in DMME
5. Conclusion5. Conclusion
1. Introduction1. Introduction
2. Climatological map of DEMETER 7 models 2. Climatological map of DEMETER 7 models
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
PeriodPeriod 1980 yr ~ 2001 yr (Summer mean/Winter mean)1980 yr ~ 2001 yr (Summer mean/Winter mean) Region Region
Lon. : 40E~160E , Lat. : 20S~60NLon. : 40E~160E , Lat. : 20S~60N
Variable Variable Precipitation , 2m TemperaturePrecipitation , 2m Temperature
1. Introduction1. Introduction
CERCERFF
ECMECMWW
INGINGVV
LODLODYY
MAXMAXPP
METMETFF
UKMUKMOO
DMMDMMEE
OBSOBS
850 hPa wind climatology (JJA)850 hPa wind climatology (JJA)
2. Climatological structure of DEMETER models2. Climatological structure of DEMETER models
CERCERFF
ECMECMWW
INGINGVV
LODLODYY
MAXMAXPP
METMETFF
UKMUKMOO
DMMDMMEE
OBSOBS
2m Temperature climatology (JJA)2m Temperature climatology (JJA)
2. Climatological structure of DEMETER models2. Climatological structure of DEMETER models
Precipitation climatology (JJA)Precipitation climatology (JJA)
2. Climatological structure of DEMETER models2. Climatological structure of DEMETER models
CERCERFF
ECMECMWW
INGINGVV
LODLODYY
MAXMAXPP
METMETFF
UKMUKMOO
DMMDMMEE
OBSOBS
Correlation between observation and MME of Precipitation Correlation between observation and MME of Precipitation
observation and MME of Precipitation over Northeast Chinaobservation and MME of Precipitation over Northeast China
observation and MME of Precipitation over Mid-lower observation and MME of Precipitation over Mid-lower Yangtze River basinsYangtze River basins
2. Climatological structure of DEMETER models2. Climatological structure of DEMETER models
Effect of MME Effect of MME : Mean Bias reduction : Mean Bias reduction
CMAP climatology – ECMW model climatologyCMAP climatology – ECMW model climatology
CMAP climatology – Multi-model climatology CMAP climatology – Multi-model climatology
3. Deterministic Forecast skill in MME3. Deterministic Forecast skill in MME
Correlation skill between Observation and Multi-Model Correlation skill between Observation and Multi-Model
MSLP MSLP JJAJJA
DJFDJF
PRCP PRCP JJAJJA
DJFDJF
TA2M TA2M JJAJJA
DJFDJF
3. Deterministic Forecast skill in MME3. Deterministic Forecast skill in MME
Indian ocean index Indian ocean index JJAJJA
DJFDJF
The Indian Ocean The Indian Ocean RegionRegion
Lon. : 40 E ~ 110 ELon. : 40 E ~ 110 E
Lat. : 15 S ~ 10 NLat. : 15 S ~ 10 N
Var. : SST anomalyVar. : SST anomaly
Black line : Black line : Observation indexObservation index
Red line : the index in Red line : the index in DMMEDMME
3. Deterministic Forecast skill in MME3. Deterministic Forecast skill in MME
East Asia Summer Monsoon index East Asia Summer Monsoon index
The East Asia RegionThe East Asia Region
Black line : Observation Black line : Observation indexindex
Green line : the index in Green line : the index in DMMEDMME
)500:(
):(sin
45sin
)125,20(25.0
)125,40(50.0
)125,60(25.0
heightlgeopotentahPaZZZZ
latitudeZZ
ENZ
ENZ
ENZEASM
s
s
s
s
Correlation between EASM Index and Precipitation Correlation between EASM Index and Precipitation
Observation(left) MME(right)
Observation(left) MME(right)
Precipitation in strong monsoon year(1997)Precipitation in strong monsoon year(1997)
Observation(left) MME(right)
Precipitation in weak monsoon year(1998)Precipitation in weak monsoon year(1998)
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
First Step : Climatological Probability Distribution Function
Climatological PDF
0 Xc-Xc
Second Step : Probability Forecast for particular time
- Normalizing all the forecast value )1,0(~),( NxZ
• In the 3 category case, -Xc and Xc make the below area separate 1/3 value each.
Ensemble PDF of particular time
BN NN AN
Below normal (BN)
Near normal (NN)
Above normal (AN)
Non-parametric approach
Parametric approach
dotstotal
dotsred
N
nP AAN
),(1
XcAP mGP
/ For Above normal case /
m : Ensemble mean value for particular year
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
TS2M PRCP
1982 winter mean
1985 winter mean
Reliability diagramReliability diagram: graphically represent the performance of probability forecasts of
dichotomous events for each category
The plot of observed relative frequency as a function of forecast probability :
The 1:1 diagonal perfect reliability line : A summary of the frequency of use of each forecast value
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
qqf )(
qagainstqfofvaluethe )(
Black, dashed line : Each Black, dashed line : Each modelmodel
Red, solid line : DMMERed, solid line : DMME
Above Normal Category ( Global Above Normal Category ( Global Region )Region )
Precipitation / JJAPrecipitation / JJA
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
Brier Score (B)Brier Score (B)
Brier skill score (BSS)Brier skill score (BSS)
n : the number of realizations of the forecasts over
which the validation is preformed
For each realization i ,
pi : forecast probability of the occurrence of the event
vi : a value equal to 1 or 0
depending on the event occurred / not.
refB
BBSS 1
Bref : a reference forecast
(taken to be the low-skill climatological forecasts)
BSS = 1 : a perfect forecast system
BSS = 0 (negative) : performs like (poorer than) the reference system
n
iii vp
nB
1
2)(1
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
CERCERFF
ECMECMWW
INGINGVV
LODLODYY
MAXMAXPP
METMETFF
UKMUKMOO
Above Normal Category Above Normal Category
Precipitation / JJAPrecipitation / JJA
DMMDMMEE
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
L
Cr
roro
orophorpfroV tt
,),min(
)1()()1()(),min(
Economic valueEconomic value
Observation (real event)
Yes No
Forecast(Action)
YesHit (h)
Cost (C)False (f)Cost (C)
NoMiss (m)Loss (L)
Correct reject
0
),(min, oL
CE
L
CoE
EE
EEV
mcliperf
perfimlc
fcstimcl
V = 1 : a perfect forecast system
V = 0 : performs like the reference system
* pt : threshold probability
4. Probabilistic Forecast skill in DMME4. Probabilistic Forecast skill in DMME
CERCERFF
ECMECMWW
INGINGVV
LODLODYY
MAXMAXPP
METMETFF
UKMUKMOO
Above Normal Category Above Normal Category
Precipitation / JJAPrecipitation / JJA
DMMDMMEE
The Multi-model shows the better predictability than the single model following this study.
But, the forecast skill is different about the variables and the target region. This is the same results as in the deterministic forecast.
Probability forecasts show more information for users about future climate than deterministic forecast. Because this contains the uncertainty in the forecast problem.
5. Conclusion5. Conclusion
Thank you !! ^o^Thank you !! ^o^