1Institute of Marine and Atmospheric Research Utrecht, Utrecht University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
2Leibniz Institute for Baltic Sea Research Warnemünde, Seestrasse 15, 18119 Rostock, Germany
3Department of Computer Science, VU University Amsterdam, 1081 HV Amsterdam, the Netherlands
4Netherlands eScience Center, 1098 XG Amsterdam, the Netherlands
Received: 18 Jul 2016 – Discussion started: 02 Aug 2016
Abstract. An important contribution to future changes in regional sea level extremes is due to the changes in intrinsic ocean variability, in particular ocean eddies. Here, we study a scenario of future dynamic sea level (DSL) extremes using a high-resolution version of the Parallel Ocean Program and generalized extreme value theory. This model is forced with atmospheric fluxes from a coupled climate model which has been integrated under the IPCC-SRES-A1B scenario over the period 2000–2100. Changes in 10-year return time DSL extremes are very inhomogeneous over the globe and are related to changes in ocean currents and corresponding regional shifts in ocean eddy pathways. In this scenario, several regions in the North Atlantic experience an increase in mean DSL of up to 0.4 m over the period 2000–2100. DSL extremes with a 10-year return time increase up to 0.2 m with largest values in the northern and eastern Atlantic.
Revised: 07 Dec 2016 – Accepted: 17 Dec 2016 – Published: 20 Jan 2017
Brunnabend, S.-E., Dijkstra, H. A., Kliphuis, M. A., Bal, H. E., Seinstra, F., van Werkhoven, B., Maassen, J., and van Meersbergen, M.: Changes in extreme regional sea level under global warming, Ocean Sci., 13, 47-60, doi:10.5194/os-13-47-2017, 2017.