The role of beach morphology on coastal cliff erosion under extreme waves
Erosion of hard-rock coastal cliffs is understood to be caused by a combination of both marine and sub-aerial processes. Beach morphology, tidal elevation and significant wave heights, especially under extreme storm conditions, can lead to variability in wave energy flux to the cliff-toe. Wave and w...
Published in: | Earth Surface Processes and Landforms |
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:107956 2023-06-11T04:14:37+02:00 The role of beach morphology on coastal cliff erosion under extreme waves Earlie, Claire Masselink, Gerd Russell, Paul 2018-05-31 application/pdf https://orca.cardiff.ac.uk/id/eprint/107956/ https://doi.org/10.1002/esp.4308 https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf en eng Wiley https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf Earlie, Claire https://orca.cardiff.ac.uk/view/cardiffauthors/A2298837S.html orcid:0000-0001-8806-3062 orcid:0000-0001-8806-3062, Masselink, Gerd and Russell, Paul 2018. The role of beach morphology on coastal cliff erosion under extreme waves. Earth Surface Processes and Landforms 43 (6) , pp. 1213-1228. 10.1002/esp.4308 https://doi.org/10.1002/esp.4308 file https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf doi:10.1002/esp.4308 cc_by Article PeerReviewed 2018 ftunivcardiff https://doi.org/10.1002/esp.4308 2023-05-04T22:34:55Z Erosion of hard-rock coastal cliffs is understood to be caused by a combination of both marine and sub-aerial processes. Beach morphology, tidal elevation and significant wave heights, especially under extreme storm conditions, can lead to variability in wave energy flux to the cliff-toe. Wave and water level measurements in the nearshore under energetic conditions are difficult to obtain and in-situ observations are rare. Here we use monthly cliff-face volume changes detected using terrestrial laser scanning alongside beach morphological changes and modelled nearshore hydrodynamics to examine how exposed cliffs respond to changes in extreme wave conditions and beach morphology. The measurements cover the North Atlantic storms of 2013-2014 and consider two exposed stretches of coastline (Porthleven and Godrevy, UK) with contrasting beach morphology fronting the cliffs; a flat dissipative sandy beach at Godrevy and a steep reflective gravel beach at Porthleven. Beach slope and the elevation of the beach-cliff junction were found to influence the frequency of cliff inundation and the power of wave-cliff impacts. Numerical modelling (XBeach-G) showed that under highly energetic wave conditions, i.e. those that occurred in the North Atlantic during winter 2013–2014, with Hs = 5.5 m (dissipative site) and 8 m (reflective site), the combination of greater wave height and steeper beach at the reflective site led to amplified wave run-up, subjecting these cliffs to waves over 4 times as powerful as those impacting the cliffs at the dissipative site (39 kWm-1 compared with 9 kWm-1). This study highlighted the sensitivity of cliff erosion to extreme wave conditions, where the majority (over 90% of the annual value) of cliff-face erosion ensued during the winter. The significance of these short-term erosion rates in the context of long-term retreat illustrates the importance of incorporating short-term beach and wave dynamics into geomorphological studies of coastal cliff change. Article in Journal/Newspaper North Atlantic Cardiff University: ORCA (Online Research @ Cardiff) Sandy Beach ENVELOPE(-55.731,-55.731,49.917,49.917) Earth Surface Processes and Landforms 43 6 1213 1228 |
institution |
Open Polar |
collection |
Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
English |
description |
Erosion of hard-rock coastal cliffs is understood to be caused by a combination of both marine and sub-aerial processes. Beach morphology, tidal elevation and significant wave heights, especially under extreme storm conditions, can lead to variability in wave energy flux to the cliff-toe. Wave and water level measurements in the nearshore under energetic conditions are difficult to obtain and in-situ observations are rare. Here we use monthly cliff-face volume changes detected using terrestrial laser scanning alongside beach morphological changes and modelled nearshore hydrodynamics to examine how exposed cliffs respond to changes in extreme wave conditions and beach morphology. The measurements cover the North Atlantic storms of 2013-2014 and consider two exposed stretches of coastline (Porthleven and Godrevy, UK) with contrasting beach morphology fronting the cliffs; a flat dissipative sandy beach at Godrevy and a steep reflective gravel beach at Porthleven. Beach slope and the elevation of the beach-cliff junction were found to influence the frequency of cliff inundation and the power of wave-cliff impacts. Numerical modelling (XBeach-G) showed that under highly energetic wave conditions, i.e. those that occurred in the North Atlantic during winter 2013–2014, with Hs = 5.5 m (dissipative site) and 8 m (reflective site), the combination of greater wave height and steeper beach at the reflective site led to amplified wave run-up, subjecting these cliffs to waves over 4 times as powerful as those impacting the cliffs at the dissipative site (39 kWm-1 compared with 9 kWm-1). This study highlighted the sensitivity of cliff erosion to extreme wave conditions, where the majority (over 90% of the annual value) of cliff-face erosion ensued during the winter. The significance of these short-term erosion rates in the context of long-term retreat illustrates the importance of incorporating short-term beach and wave dynamics into geomorphological studies of coastal cliff change. |
format |
Article in Journal/Newspaper |
author |
Earlie, Claire Masselink, Gerd Russell, Paul |
spellingShingle |
Earlie, Claire Masselink, Gerd Russell, Paul The role of beach morphology on coastal cliff erosion under extreme waves |
author_facet |
Earlie, Claire Masselink, Gerd Russell, Paul |
author_sort |
Earlie, Claire |
title |
The role of beach morphology on coastal cliff erosion under extreme waves |
title_short |
The role of beach morphology on coastal cliff erosion under extreme waves |
title_full |
The role of beach morphology on coastal cliff erosion under extreme waves |
title_fullStr |
The role of beach morphology on coastal cliff erosion under extreme waves |
title_full_unstemmed |
The role of beach morphology on coastal cliff erosion under extreme waves |
title_sort |
role of beach morphology on coastal cliff erosion under extreme waves |
publisher |
Wiley |
publishDate |
2018 |
url |
https://orca.cardiff.ac.uk/id/eprint/107956/ https://doi.org/10.1002/esp.4308 https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf |
long_lat |
ENVELOPE(-55.731,-55.731,49.917,49.917) |
geographic |
Sandy Beach |
geographic_facet |
Sandy Beach |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf Earlie, Claire https://orca.cardiff.ac.uk/view/cardiffauthors/A2298837S.html orcid:0000-0001-8806-3062 orcid:0000-0001-8806-3062, Masselink, Gerd and Russell, Paul 2018. The role of beach morphology on coastal cliff erosion under extreme waves. Earth Surface Processes and Landforms 43 (6) , pp. 1213-1228. 10.1002/esp.4308 https://doi.org/10.1002/esp.4308 file https://orca.cardiff.ac.uk/id/eprint/107956/8/esp.4308.pdf doi:10.1002/esp.4308 |
op_rights |
cc_by |
op_doi |
https://doi.org/10.1002/esp.4308 |
container_title |
Earth Surface Processes and Landforms |
container_volume |
43 |
container_issue |
6 |
container_start_page |
1213 |
op_container_end_page |
1228 |
_version_ |
1768392745880125440 |