Abstract

AbstractParameters in climate models are usually calibrated manually, exploiting only small subsets of the available data. This precludes both optimal calibration and quantification of uncertainties. Traditional Bayesian calibration methods that allow uncertainty quantification are too expensive for climate models; they are also not robust in the presence of internal climate variability. For example, Markov chain Monte Carlo (MCMC) methods typically require model runs and are sensitive to internal variability noise, rendering them infeasible for climate models. Here we demonstrate an approach to model calibration and uncertainty quantification that requires only model runs and can accommodate internal climate variability. The approach consists of three stages: (a) a calibration stage uses variants of ensemble Kalman inversion to calibrate a model by minimizing mismatches between model and data statistics; (b) an emulation stage emulates the parameter‐to‐data map with Gaussian processes (GP), using the model runs in the calibration stage for training; (c) a sampling stage approximates the Bayesian posterior distributions by sampling the GP emulator with MCMC. We demonstrate the feasibility and computational efficiency of this calibrate‐emulate‐sample (CES) approach in a perfect‐model setting. Using an idealized general circulation model, we estimate parameters in a simple convection scheme from synthetic data generated with the model. The CES approach generates probability distributions of the parameters that are good approximations of the Bayesian posteriors, at a fraction of the computational cost usually required to obtain them. Sampling from this approximate posterior allows the generation of climate predictions with quantified parametric uncertainties.

Highlights

  • Calibrating climate models with available data and quantifying their uncertainties are essential to make climate predictions accurate and actionable

  • We show how uncertainties in climate model parameters can be translated into quantified uncertainties of climate predictions through ensemble integrations

  • To check for Ensemble Kalman inversion (EKI) convergence, we evaluate an additional 4 EKI iterations

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Summary

Introduction

Calibrating climate models with available data and quantifying their uncertainties are essential to make climate predictions accurate and actionable. The principal uncertainties in climate predictions arise from the representation of unresolvable yet important small-scale processes, such as those controlling cloud cover [13, 14, 10, 83, 9, 87, 88, 12, 81]. These processes are represented by parameterization schemes, which relate unresolved quantities such as cloud statistics to variables resolved on the climate models’ computational grid, such as temperature and humidity. Some broader-scale automated approaches that more systematically quantify the plausible range of parameters have begun to be explored [19, 40]

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