Abstract
Salt marshes often undergo rapid changes in lateral extent, the causes of which lack common explanation. We combine hydrological, sedimentological, and climatological data with analysis of historical maps and photographs to show that long-term patterns of lateral marsh change can be explained by large-scale variation in sediment supply and its wave-driven transport. Over 150 years, northern marshes in Great Britain expanded while most southern marshes eroded. The cause for this pattern was a north to south reduction in sediment flux and fetch-driven wave sediment resuspension and transport. Our study provides long-term and large-scale evidence that sediment supply is a critical regulator of lateral marsh dynamics. Current global declines in sediment flux to the coast are likely to diminish the resilience of salt marshes and other sedimentary ecosystems to sea level rise. Managing sediment supply is not common place but may be critical to mitigating coastal impacts from climate change.
| Original language | English |
|---|---|
| Pages (from-to) | 11178-11187 |
| Number of pages | 10 |
| Journal | Geophysical Research Letters |
| Volume | 46 |
| Issue number | 20 |
| DOIs | |
| Publication status | Published - 28 Oct 2019 |
Funding
This research was supported by Coleg Cymraeg Cenedlaethol to C. J. T. L., by the Welsh Government and Higher Education Funding Council for Wales through Sêr Cymru National Research Network for Low Carbon, Energy and Environment to M. F. D.‐E., J. F. P., T. J. B., and M. W. S., by the Natural Environment Research Council (NERC) C‐SIDE Grant NE/R010846/1 to C. J. T. L. and M. W. S., and by the Nederlandse Organisatie voor Wetenschappelijk Onderzoek (NWO) BE‐SAFE Grant 850.13.011 and TTW AllRisk (P21.2 project B) for financial support in understanding the use of salt marshes for coastal defense to T. J. B. We thank Prof. Tom Spencer from Cambridge University and Dr Jonathan Malarkey, Prof. Jaco Baas, Prof. Hilary Kennedy, and Prof. Stuart Jenkins from Bangor University for their constructive comments. The GIS layers showing change in marsh extent and the variables used in the statistical analysis for this study are accessible via the Environmental Information Data Centre repository (DOI: 10.5285/03b62fd0‐41e2‐4355‐9a06‐1697117f0717). The authors declare no conflict of interest.
Keywords
- lateral saltmarsh dynamics
- sea level rise
- sediment supply
- wave fetch