Abstract

Denmark has a long, complex coastline, connecting the North Sea in the west to the semi-enclosed Baltic Sea in the east, via the Skagerrak-Kattegat Seas. Historical sea level records indicate that relative sea level (RSL) has been increasing along the Danish North Sea coast, south of Skagerrak, following the global mean sea level (GMSL) rise. In the central Skagerrak-Kattegat Seas, RSL rise has been practically absent, due to the GMSL rise being off-set by the Fennoscandian post-glacial land-uplift. The new IPCC Special Report on the Ocean and Cryosphere in a Changing Climate (SROCC) reported that under RCP8.5 GMSL will increase more than the previous estimates in the IPCC Fifth Assessment Report (AR5) at the end of twenty-first century due to Antarctic ice sheet dynamics. We performed a regionalization of the SROCC sea level projections for the “Danish Climate Atlas” dataset, a nation-wide climate adaptation dataset based on IPCC and various national and international databases. In these complementary datasets, important local data have been considered, which have not been included in the IPCC SROCC GMSL rise estimates, i.e., more precise national-wide land-rise prediction and sets of sea level fingerprints. Our results indicate that sea level projections under RCP8.5 results in a > 40 cm RSL rise at the end of the twenty-first century in the Skagerrak-Kattegat Seas, which might call for a new adaptation strategy in this region. The rate of mean sea level rise will exceed the rate of the land-rise earlier than the previous estimates by AR5 under the RCP8.5 scenario. In particular, we stress how these new estimates will affect future extreme sea levels in this region. Based on our results, we suggest this more recent GMSL projection needs to be considered in coastal risk assessments in the Skagerrak-Kattegat Seas also in this century.

Highlights

  • Adapting to climate change, especially to sea level rise (SLR), in the coastal region is an ongoing challenge for policy-makers and into the future (Moser and Ekstrom, 2010)

  • One of the essential questions for SLR in the SkagerrakKattegat Seas is whether the location of the neutral SLR zone will remain, or else how it will shift in the future

  • In the middle of the twenty-first century, the median value of the rate of relative sea level (RSL) rise already shows that the Skagerrak-Kattegat Seas are within the positive SLR zone, and it will accelerate in the half of the twenty-first century

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Summary

Introduction

Especially to sea level rise (SLR), in the coastal region is an ongoing challenge for policy-makers and into the future (Moser and Ekstrom, 2010). The Danish Climate Atlas project was designed to provide climate service by establishing a go-to platform for climate information, based on the production of a consistent, nation-wide and accessible data set, which is maintained and regularly updated. Pioneering projects assessing the users’ needs for sea level rise information within the Copernicus Climate Change Service framework, further accentuates that it is of vital importance for coastal planning and adaptation purposes that reliable and robust, upto-date information on SLR, and the impacts of extreme sea level events, are updated regularly (1–5 years, Madsen et al, 2019b; Muis et al, 2020)

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