A national coastal erosion susceptibility model for Scotland

James M. Fitton*, Jim D. Hansom, Alistair F. Rennie

*Corresponding author for this work

Research output: Contribution to journalJournal articleResearchpeer-review

39 Citations (Scopus)

Abstract

The upland nature of the Scottish landscape means that much of the social and economic activity has a coastal bias. The importance of the coast is further highlighted by the wide range of ecosystem services that coastal habitats provide. It follows that the threat posed by coastal erosion and flooding has the potential to have a substantial effect on the socioeconomic activity of the whole country. Currently, the knowledge base of coastal erosion is poor and this serves to hinder the current and future management of the coast. To address this knowledge gap, two interrelated models have been developed and are presented here: the Underlying Physical Susceptibility Model (UPSM) and the Coastal Erosion Susceptibility Model (CESM). The UPSM is generated within a GIS at a 50 m2 raster of national coverage, using data relating to ground elevation, rockhead elevation, wave exposure and proximity to the open coast. The CESM moderates the outputs of the UPSM to include the effects of sediment supply and coastal defence data. When validated against locations in Scotland that are currently experiencing coastal erosion, the CESM successfully identifies these areas as having high susceptibility. This allows the UPSM and CESM to be used as tools to identify assets inherently exposed to coastal erosion, areas where coastal erosion may exacerbate coastal flooding, and areas are inherently resilient to erosion, thus allow more efficient and effective management of the Scottish coast.

Original languageEnglish
JournalOcean and Coastal Management
Volume132
Pages (from-to)80-89
Number of pages10
ISSN0964-5691
DOIs
Publication statusPublished - 1 Nov 2016
Externally publishedYes

Keywords

  • Coastal erosion
  • Coastal management
  • GIS
  • Physical susceptibility
  • Scotland

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