A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK

Recession of coastal cliffs (bluffs) is a significant problem globally, as around 80% of Earth’s coastlines are classified as sea cliffs. It has long been recognised that beaches control wave energy dissipation on the foreshore and, as a result, can provide protection from shoreline and cl...

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Main Authors: Pablo Muñoz López, Andrés Payo, Michael A. Ellis, Francisco Criado-Aldeanueva, Gareth Owen Jenkins
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/8/1/20
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author Pablo Muñoz López
Andrés Payo
Michael A. Ellis
Francisco Criado-Aldeanueva
Gareth Owen Jenkins
author_facet Pablo Muñoz López
Andrés Payo
Michael A. Ellis
Francisco Criado-Aldeanueva
Gareth Owen Jenkins
author_sort Pablo Muñoz López
collection DOAJ
description Recession of coastal cliffs (bluffs) is a significant problem globally, as around 80% of Earth’s coastlines are classified as sea cliffs. It has long been recognised that beaches control wave energy dissipation on the foreshore and, as a result, can provide protection from shoreline and cliff erosion. However, there have been few studies that have quantified the relationship between beach levels and cliff recession rates. One of the few quantitative studies has shown that there is a measurable relationship between the beach thickness (or beach wedge area (BWA) as a proxy for beach thickness) and the annual cliff top recession rate along the undefended coast of North Norfolk and Suffolk in eastern England, United Kingdom (UK). Additionally, previous studies also found that for profiles with low BWA, the annual cliff top recession rate frequency distribution follows a bimodal distribution. This observation suggests that as BWA increases, not only does cliff top recession rate become lower, but also more predictable, which has important implications for coastal stakeholders particularly for planning purposes at decadal and longer time scales. In this study, we have addressed some of the limitations of the previous analysis to make it more transferable to other study sites and applicable to longer time scales. In particular, we have automatised the extraction of cliff tops, toe locations, and BWA from elevation profiles. Most importantly, we have verified the basic assumption of space-for-time substitution in three different ways: (1) Extending the number or years analysed in a previous study from 11 to 24 years, (2) extending the number of locations at which cliff top recession rate and BWA are calculated, and (3) exploring the assumption of surface material remaining unchanged over time by using innovative 3D subsurface modelling. The present study contributes to our understanding of a poorly known aspect of cliff−beach interaction and outlines a quantitative approach that allows for simple analysis of widely available topographical elevation profiles, enabling the extraction of measurable indicators of coastal erosion.
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spelling doaj.art-d178a44b910143869f72856c122c44a12022-12-21T18:48:48ZengMDPI AGJournal of Marine Science and Engineering2077-13122020-01-01812010.3390/jmse8010020jmse8010020A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UKPablo Muñoz López0Andrés Payo1Michael A. Ellis2Francisco Criado-Aldeanueva3Gareth Owen Jenkins4British Geological Survey, Keyworth, Nottingham NG12 5GG, UKBritish Geological Survey, Keyworth, Nottingham NG12 5GG, UKBritish Geological Survey, Keyworth, Nottingham NG12 5GG, UKPhysical Oceanography Group, Department of Applied Physics II, University of Málaga, 29071 Málaga, SpainBritish Geological Survey, Keyworth, Nottingham NG12 5GG, UKRecession of coastal cliffs (bluffs) is a significant problem globally, as around 80% of Earth’s coastlines are classified as sea cliffs. It has long been recognised that beaches control wave energy dissipation on the foreshore and, as a result, can provide protection from shoreline and cliff erosion. However, there have been few studies that have quantified the relationship between beach levels and cliff recession rates. One of the few quantitative studies has shown that there is a measurable relationship between the beach thickness (or beach wedge area (BWA) as a proxy for beach thickness) and the annual cliff top recession rate along the undefended coast of North Norfolk and Suffolk in eastern England, United Kingdom (UK). Additionally, previous studies also found that for profiles with low BWA, the annual cliff top recession rate frequency distribution follows a bimodal distribution. This observation suggests that as BWA increases, not only does cliff top recession rate become lower, but also more predictable, which has important implications for coastal stakeholders particularly for planning purposes at decadal and longer time scales. In this study, we have addressed some of the limitations of the previous analysis to make it more transferable to other study sites and applicable to longer time scales. In particular, we have automatised the extraction of cliff tops, toe locations, and BWA from elevation profiles. Most importantly, we have verified the basic assumption of space-for-time substitution in three different ways: (1) Extending the number or years analysed in a previous study from 11 to 24 years, (2) extending the number of locations at which cliff top recession rate and BWA are calculated, and (3) exploring the assumption of surface material remaining unchanged over time by using innovative 3D subsurface modelling. The present study contributes to our understanding of a poorly known aspect of cliff−beach interaction and outlines a quantitative approach that allows for simple analysis of widely available topographical elevation profiles, enabling the extraction of measurable indicators of coastal erosion.https://www.mdpi.com/2077-1312/8/1/20cliff behaviourcliff recessionerosionbeach wedge area (bwa)space-for-time substitutionergodic system
spellingShingle Pablo Muñoz López
Andrés Payo
Michael A. Ellis
Francisco Criado-Aldeanueva
Gareth Owen Jenkins
A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
Journal of Marine Science and Engineering
cliff behaviour
cliff recession
erosion
beach wedge area (bwa)
space-for-time substitution
ergodic system
title A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
title_full A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
title_fullStr A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
title_full_unstemmed A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
title_short A Method to Extract Measurable Indicators of Coastal Cliff Erosion from Topographical Cliff and Beach Profiles: Application to North Norfolk and Suffolk, East England, UK
title_sort method to extract measurable indicators of coastal cliff erosion from topographical cliff and beach profiles application to north norfolk and suffolk east england uk
topic cliff behaviour
cliff recession
erosion
beach wedge area (bwa)
space-for-time substitution
ergodic system
url https://www.mdpi.com/2077-1312/8/1/20
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