Impacts of Antarctic fast dynamics on sea-level projections and coastal flood defense
Tony E. Wong, Alexander M.R. Bakker, Klaus Keller

TL;DR
This paper assesses the potential impact of rapid Antarctic ice sheet disintegration on sea-level rise projections and coastal flood defenses, emphasizing the importance of including this uncertainty in risk management strategies.
Contribution
It introduces a probabilistic framework to estimate the contribution of Antarctic fast dynamics to sea-level rise and explores its implications for coastal flood defense planning.
Findings
Fast Antarctic disintegration could cause 21-74 cm sea-level rise this century.
Neglecting fast dynamics leads to underprepared flood defense strategies.
Including fast dynamics increases the estimated costs and risk mitigation needs.
Abstract
Strategies to manage the risks posed by future sea-level rise hinge on a sound characterization of the inherent uncertainties. One of the major uncertainties is the possible rapid disintegration of large fractions of the Antarctic ice sheet in response to rising global temperatures. This could potentially lead to several meters of sea-level rise during the next few centuries. Previous studies have typically been silent on two coupled questions: (i) What are probabilistic estimates of this "fast dynamics" contribution to sea-level rise? (ii) What are the implications for strategies to manage coastal flooding risks? Here, we present probabilistic hindcasts and projections of sea-level rise to 2100. The fast dynamics mechanism is approximated by a simple parameterization, designed to allow for a careful quantification of the uncertainty in its contribution to sea-level rise. We estimate…
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