advanced uncertainty evaluation of climate models and their future climate projections

19
Advanced uncertainty evaluation of climate models and their future climate projections H Järvinen, P Räisänen , M Laine, J Tamminen, P Ollinaho Finnish Meteorological Institute A Ilin, E Oja Aalto University School of Science and Technology , Finland A Solonen, H Haario Lappeenranta University of Technology, Finland

Upload: lavada

Post on 09-Jan-2016

27 views

Category:

Documents


0 download

DESCRIPTION

Advanced uncertainty evaluation of climate models and their future climate projections H Järvinen, P Räisänen , M Laine, J Tamminen, P Ollinaho Finnish Meteorological Institute A Ilin, E Oja Aalto University School of Science and Technology , Finland A Solonen, H Haario - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Advanced uncertainty evaluation of climate models and their future climate projections

Advanced uncertainty evaluation of climate models and their future climate

projections

H Järvinen, P Räisänen, M Laine, J Tamminen, P OllinahoFinnish Meteorological Institute

A Ilin, E OjaAalto University School of Science and Technology , Finland

A Solonen, H HaarioLappeenranta University of Technology, Finland

Page 2: Advanced uncertainty evaluation of climate models and their future climate projections

Closure parameters• Appear in physical parameterization schemes where

some unresolved variables are expressed by predefined parameters rather than being explicitly modelled

• Span a low-dimensional non-linear estimation problem

• Currently: best expert knowledge is used to specify the optimal closure parameter values, based on observations, process studies, model simulations, etc.

• Important when:

(1) Fine-tuning climate models to the present climate

(2) Replacing parameterization schemes with new ones

2/19

Page 3: Advanced uncertainty evaluation of climate models and their future climate projections

3/19

Markov chain Monte Carlo (MCMC) • Consecutive model simulations while updating the

model parameters by Monte Carlo sampling

• Proposal step (parameter values drawn from a proposal distribution)

• Acceptance step (evaluate the objective function and accept/reject the proposal)

• “A random walk” in the parameter space (a Markov chain) and exploration of the Bayesian posterior distribution

• Not optimization ... Instead, a full multi-dimensional parameter probability distribution is recovered

Page 4: Advanced uncertainty evaluation of climate models and their future climate projections

4/19

MH (non-adaptive)

AM

DRAM (adaptive)

Page 5: Advanced uncertainty evaluation of climate models and their future climate projections

ECHAM5 closure parameters

CAULOC = influencing the autoconversion of cloud droplets (rain formation, stratiform clouds)

CMFCTOP = relative cloud mass flux at level above non-buoyancy (in cumulus mass flux

scheme)

CPRCON = a coefficient for determining conversion from cloud water to rain (in convective

clouds)

ENTRSCV = entrainment rate for shallow convection5/19

Page 6: Advanced uncertainty evaluation of climate models and their future climate projections

ECHAM5 simulations

• Markov chain in the 4-parameter space

• One year simulation with the T21L19 ECHAM5 model repeated many times with perturbed parameters

• Several objective function were tested

• All formulations: Top-of-Atmosphere (ToA) net radiative flux

6/19

Page 7: Advanced uncertainty evaluation of climate models and their future climate projections

7/19

cost 2

2

modelGLOBAL

obs

obsFF

Global-annual mean net flux in ECHAM5

Global-annual mean net flux in CERES data (0.9 W m-2)

Interannual standard deviationIn ERA40 reanalysis (0.53 Wm-2)

2

2obs,model,

12

1t121

costZONAL

yt

ytyt

yy

FFw

Monthly zonal-mean values

Interannual std. dev. of monthly zonal means

Page 8: Advanced uncertainty evaluation of climate models and their future climate projections

8/19

cost 2

2

modelGLOBAL

obs

obsFF

Global-annual mean net flux in ECHAM5

Global-annual mean net flux in CERES data (0.9 W m-2)

Interannual standard deviationIn ERA40 reanalysis (0.53 Wm-2)

2

2obs,model,

12

1t121

costZONAL

yt

ytyt

yy

FFw

Monthly zonal-mean values

Interannual std. dev. of monthly zonal means

Small cost function implies model to be close to CERES data

- global annual-mean net radiation

- annual cycle of zonal mean net radiation

Page 9: Advanced uncertainty evaluation of climate models and their future climate projections

9/19

Longwave Shortwave

CERES observations

Global annual mean ToA radiative flux

Net

• cost =costGLOBAL + costZONAL

Page 10: Advanced uncertainty evaluation of climate models and their future climate projections

10/19

Longwave Shortwave

Default model

Net

• cost =costGLOBAL + costZONAL

Page 11: Advanced uncertainty evaluation of climate models and their future climate projections

11/19

Longwave Shortwave

The cost function only included net ToA radiation…

both the LW and SW biases decreased

Net

Page 12: Advanced uncertainty evaluation of climate models and their future climate projections
Page 13: Advanced uncertainty evaluation of climate models and their future climate projections

= default value

Page 14: Advanced uncertainty evaluation of climate models and their future climate projections

T42L31 :: Cloud ice particles, SW scattering

14/19

CAULOC CMFCTOP CPRCON ENTRSCV

CPRCON ENTRSCVCMFCTOP ZASICCAULOC ZINPAR ZINHOMI

Page 15: Advanced uncertainty evaluation of climate models and their future climate projections

Uncertainty of future climate projections (principle)

• Climate sensitivity :: Change in Tsurf due to 2 × CO2

• Sample from the closure parameter posterior PDF’s

• Perform a climate sensitivity run with each model

• Result: a proper PDF of climate sensitivity

- conditional on the selected closure parameters and cost function

15/19

Page 16: Advanced uncertainty evaluation of climate models and their future climate projections

Practical problem: at T21L19, ECHAM5 is hypersensitive!

16/19

Warming 8.9 Kwhen model crashes!

Warming 9.6 Kwhen model crashes!!

Glo

bal-m

ean

tem

pera

ture

(K

)

Page 17: Advanced uncertainty evaluation of climate models and their future climate projections

Conclusions (so far)

17/19

Can we use MCMC for parameter estimation in climate models?

Yes, we can! But …

2) It is computationally expensive - chain lengths of > 1000 model runs are needed

1) Choice of the cost function is critical

Page 18: Advanced uncertainty evaluation of climate models and their future climate projections

Means to fight the computational expense• Adaptive MCMC

• parallel MCMC chains ( reduced wallclock time)

• re-use of chains (off-line tests of new cost functions through ”importance sampling”)

• Early rejection scheme …

18/19Month

Rejection limit

Page 19: Advanced uncertainty evaluation of climate models and their future climate projections

Many thanks

19/19

[email protected]

[email protected]