Ocean model resolution dependence of Caribbean sea-level projections
René M. van Westen (Universiteit Utrecht)
Henk A. Dijkstra (Universiteit Utrecht)
Carine G. van der Boog (TU Delft - Civil Engineering & Geosciences)
Caroline A. Katsman (TU Delft - Civil Engineering & Geosciences)
Rebecca K. James (Universiteit Utrecht)
Tjeerd J. Bouma (NIOZ Royal Netherlands Institute for Sea Research, Universiteit Utrecht)
Olga Kleptsova (Universiteit Utrecht)
Roland Klees (TU Delft - Civil Engineering & Geosciences)
Riccardo E.M. Riva (TU Delft - Civil Engineering & Geosciences)
D. Cornelis Slobbe (TU Delft - Civil Engineering & Geosciences)
Marcel Zijlema (TU Delft - Civil Engineering & Geosciences)
Julie D. Pietrzak (TU Delft - Civil Engineering & Geosciences)
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Abstract
Sea-level rise poses severe threats to coastal and low-lying regions around the world, by exacerbating coastal erosion and flooding. Adequate sea-level projections over the next decades are important for both decision making and for the development of successful adaptation strategies in these coastal and low-lying regions to climate change. Ocean components of climate models used in the most recent sea-level projections do not explicitly resolve ocean mesoscale processes. Only a few effects of these mesoscale processes are represented in these models, which leads to errors in the simulated properties of the ocean circulation that affect sea-level projections. Using the Caribbean Sea as an example region, we demonstrate a strong dependence of future sea-level change on ocean model resolution in simulations with a global climate model. The results indicate that, at least for the Caribbean Sea, adequate regional projections of sea-level change can only be obtained with ocean models which capture mesoscale processes.