Using salt marshes for coastal protection: Effective but hard to get where needed most

Author:

Marin‐Diaz Beatriz12ORCID,van der Wal Daphne13ORCID,Kaptein Leon2,Martinez‐Garcia Pol4,Lashley Christopher H.56ORCID,de Jong Kornelis7,Nieuwenhuis Jan Willem7,Govers Laura L.28ORCID,Olff Han2ORCID,Bouma Tjeerd J.129ORCID

Affiliation:

1. Department of Estuarine and Delta Systems NIOZ Royal Netherlands Institute for Sea Research Yerseke The Netherlands

2. Conservation Ecology Group, Groningen Institute for Evolutionary Life Sciences University of Groningen Groningen The Netherlands

3. Faculty of Geo‐Information Science and Earth Observation (ITC) University of Twente Enschede The Netherlands

4. The Fieldwork Company Groningen the Netherlands

5. Department of Hydraulic Engineering Delft University of Technology Delft The Netherlands

6. Center for Applied Coastal Research University of Delaware Newark Delaware USA

7. Regional Water Authority Noorderzijlvest Groningen The Netherlands

8. Department of Coastal Systems NIOZ Royal Netherlands Institute for Sea Research Den Burg The Netherlands

9. Faculty of Geosciences Utrecht University Utrecht The Netherlands

Abstract

Abstract Salt marshes fronting coastal structures, such as seawalls and dikes, may offer important ecosystem‐based coastal defence by reducing the wave loading and run‐up levels during storms. We question (i) how the long‐term salt marsh development in the Dutch Wadden Sea relates to the tidal‐flat foreshore bathymetry and (ii) how the wave run‐up onto dikes, which enhances the risk of dike failure, depends on foreshore bathymetry, the presence/absence of marshes, marsh vegetation properties, tidal range and wind exposure. We analysed 15 years of vegetation and bathymetry maps along the entire Dutch Wadden Sea coast, in combination with detailed process‐based measurements at five locations during 3 years, to understand where salt marshes naturally form and what features determine their contribution to coastal protection. The horizontal extent of marshes along the dikes remained relatively stable over the past decade. The presence of marshes was associated with higher elevations of adjacent tidal flats (above ~0.5 m NAP), while landward‐directed marsh retreat was associated with surface erosion of the fronting tidal flats. Wave run‐up during storms was lower at sites with wider marshes and higher foreshore elevations. This was attributed to the marsh attenuation effect, which led to a reduction in wave heights at the dike toe. As the tidal range varies across the Dutch Wadden Sea, areas to the East with generally higher water levels experienced higher wave run‐up. Synthesis and applications. We found that (i) marshes, where present, effectively protected the dikes from wave loading and (ii) the sites where marshes typically do not develop spontaneously were the most vulnerable to high wave run‐up. This catch‐22 problem implies that increasing reliance on nature‐based coastal defences along soft‐bottom coasts may require human interventions to stimulate marsh formation at the locations where it is most needed. Alternatively, ‘hard engineering’ solutions may remain necessary where implementing nature‐based solutions are either too costly, unachievable, or at the expense of other ecological values, such as causing the loss of mudflats that are important for migratory birds.

Funder

Deltares

Raymond Williams Society

Nederlandse Organisatie voor Wetenschappelijk Onderzoek

Stichting Toegepast Onderzoek Waterbeheer

Publisher

Wiley

Subject

Ecology

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