Abstract

The response of the Antarctic ice sheet (AIS) to changing global temperatures is a key component of sea-level projections. Current projections of the AIS contribution to sea-level changes are deeply uncertain. This deep uncertainty stems, in part, from (i) the inability of current models to fully resolve key processes and scales, (ii) the relatively sparse available data, and (iii) divergent expert assessments. One promising approach to characterizing the deep uncertainty stemming from divergent expert assessments is to combine expert assessments, observations, and simple models by coupling probabilistic inversion and Bayesian inversion. Here, we present a proof-of-concept study that uses probabilistic inversion to fuse a simple AIS model and diverse expert assessments. We demonstrate the ability of probabilistic inversion to infer joint prior probability distributions of model parameters that are consistent with expert assessments. We then confront these inferred expert priors with instrumental and paleoclimatic observational data in a Bayesian inversion. These additional constraints yield tighter hindcasts and projections. We use this approach to quantify how the deep uncertainty surrounding expert assessments affects the joint probability distributions of model parameters and future projections.

Highlights

  • Sea-level rise increases risks to coastal communities [1]

  • We demonstrate that probabilistic inversion leads to expert prior model parameters that are consistent with the expert assessments

  • We demonstrate how a coupled probabilistic-Bayesian inversion may be used to combine expert assessments with paleoclimatic and instrumental data in order to make probabilistic projections of future sea-level rise from the Antarctic ice sheet

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Summary

Introduction

Sea-level rise increases risks to coastal communities [1]. Approaches to managing these risks include augmenting levees, adding new flood control and shoreline protection structures, diverting sediments, improving infrastructure, relocating vulnerable populations, and restoring or enhancing natural coastal protections, such as barrier reefs, barrier islands, ridges, marshes, and regional hydrology [2,3]. The design of sound risk management strategies depends on quantifying and characterizing the uncertainties surrounding sea-level projections [4,5]. Projections of future sea-level rise depend on deeply uncertain projections of Antarctic ice sheet (AIS) mass loss [4,6,7,8,9].

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