a bayesian calibrated deglacial history for the north american ice complex
DESCRIPTION
A Bayesian Calibrated Deglacial History for the North American Ice Complex. Lev Tarasov, Radford Neal, and W. R. Peltier University of Toronto. Outline. Model Data Model + Data: Calibration methodology Some key results. Glacial modelling challenges and issues. Glacial Systems Model (GSM). - PowerPoint PPT PresentationTRANSCRIPT
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A Bayesian Calibrated Deglacial History for the North American Ice
Complex
Lev Tarasov, Radford Neal, and W. R. PeltierUniversity of Toronto
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Outline
Model Data Model + Data: Calibration methodology Some key results
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Glacial modelling challenges and issues
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Glacial Systems Model (GSM)
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Climate forcing
LGM monthly temperature and precipitation from 6 highest resolution PMIP runs
Mean and top EOFS Total of 18 ensemble
climate parameters
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Need constraints -> DATA
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Deglacial margin chronology
(Dyke, 2003) 36 time-slices +/- 50 km
uncertainty Margin buffer
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Relative sea-level (RSL) data
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VLBI and absolute gravity data
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Noisy data and non-linear system => need calibration and error bars
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Bayesian calibration
Sample over posterior probability distribution for the ensemble parameters given fits to observational data using Markov Chain Monte Carlo (MCMC) methods
Sampling also subject to additional volume and ice thickness constraints
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Large ensemble Bayesian calibration
Bayesian neural network integrates over weight space
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It works!
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RSL results, best fit models
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LGM characteristics
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LGM comparisons
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Maximum NW ice thickness
Green runs fail constraints
Blue runs pass constraints
Red runs are top 20% of blue runs
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Calibration favours fast flow
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Deglacial chronology
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Summary
Glaciological results Large Keewatin ice dome Multi-domed structure due to geographically restricted fast
flows Need strong ice calving and/or extensive ice-shelves in the
Arctic to fit RSL data Need thin time-average Hudson Bay ice to fit RSL data
Bayesian calibration method links data and physics (model) -> rational error bars
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Issues and challenges Choice of ensemble parameters
Parameter set ended up being extended with time as troublesome regions were identified
Method could easily handle more parameters, so best to try to cover deglacial phase space from the start
Challenge of identifying appropriate priors for each parameter Error model for RSL data
Noisy and likely site biased Error model allows for site scaling and time-shifting Heavy-tailed error model to limit influence of outliers
Neural network Non-trivial to find appropriate configuration Neural network for RSL was most complex: multi-layered and
separate clusters for site location and time Training takes a long time, predictions can be weak for
distant regions MCMC sampling
Can get stuck in local minima “Unphysical” solutions cropped up => added constraints
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RSL data redundancy Fairly close correspondence between fit to full RSL data set and fit
to reduced 313 datapoint calibration data set (only the last 50 runs have been calibrated against the whole data set)
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RSL data fits Data-points should
generally provide lower envelope of true RSL history
Black: best overall fit with full constraints
Red: best overall fit to 313 data set and geodetic data with full constraints
Green: best fit to just 313 RSL data, no constraints
Blue: best fit to just full RSL data, no constraints
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NA LGM ice volume Best fits required low volumes given global constraints
Possible indication of need for stronger Heinrich events
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Critical RSL site: SE Hudson Bay
Fitting this site required very strong regional desert-elevation effect (ie low value) and therefore thin and warm ice core
Atmospheric reorganization or weak Heinrich events?
Thin core results in low ice volumes
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Summary
Bayesian calibration It works but is a non-trivial exercise Need to ensure that parameter space is large enough Phase space of model deglacial history must be quite bumpy Tricky to define complete error bars Calibration had tendency to find “wacky(?)” solutions
Glaciological results Large Keewatin ice dome Multi-domed structure due to geographically restricted fast
flows Need strong ice calving and/or extensive ice-shelves in the
arctic to fit RSL data Need thin time-average Hudson Bay ice to fit RSL data
Future work: Faster (more diffusive computational kernal) ice-flow Addition of hydrological constraints and other data (especially
to better constrain south-central and NW sectors)