Physical Modelling of Arctic Coastlines—Progress and Limitations.

Permafrost coastlines represent a large portion of the world’s coastal area and these areas have become increasingly vulnerable in the face of climate change. The predominant mechanism of coastal erosion in these areas has been identified through several observational studies as thermomechanical ero...

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Published in:Water
Main Authors: Korte, Sophia, Gieschen, Rebekka, Stolle, Jacob, Goseberg, Nils
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Ice
Online Access:https://espace.inrs.ca/id/eprint/10378/
https://espace.inrs.ca/id/eprint/10378/1/P3775.pdf
https://doi.org/10.3390/w12082254
id ftinrsquebec:oai:espace.inrs.ca:10378
record_format openpolar
spelling ftinrsquebec:oai:espace.inrs.ca:10378 2023-05-15T14:25:36+02:00 Physical Modelling of Arctic Coastlines—Progress and Limitations. Korte, Sophia Gieschen, Rebekka Stolle, Jacob Goseberg, Nils 2020 application/pdf https://espace.inrs.ca/id/eprint/10378/ https://espace.inrs.ca/id/eprint/10378/1/P3775.pdf https://doi.org/10.3390/w12082254 en eng https://espace.inrs.ca/id/eprint/10378/1/P3775.pdf Korte, Sophia, Gieschen, Rebekka, Stolle, Jacob orcid:0000-0003-0902-9339 et Goseberg, Nils (2020). Physical Modelling of Arctic Coastlines—Progress and Limitations. Water , vol. 12 , nº 8. p. 2254. DOI:10.3390/w12082254 <https://doi.org/10.3390/w12082254>. doi:10.3390/w12082254 permafrost erosion coastal erosion experimental modelling Article Évalué par les pairs 2020 ftinrsquebec https://doi.org/10.3390/w12082254 2023-02-10T11:46:08Z Permafrost coastlines represent a large portion of the world’s coastal area and these areas have become increasingly vulnerable in the face of climate change. The predominant mechanism of coastal erosion in these areas has been identified through several observational studies as thermomechanical erosion—a joint removal of sediment through the melting of interstitial ice (thermal energy) and abrasion from incoming waves (mechanical energy). However, further developments are needed looking how common design parameters in coastal engineering (such as wave height, period, sediment size, etc.) contribute to the process. This paper presents the current state of the art with the objective of establishing the necessary research background to develop a process-based approach to predicting permafrost erosion. To that end, an overarching framework is presented that includes all major, erosion-relevant processes, while delineating means to accomplish permafrost modelling in experimental studies. Preliminary modelling of generations zero and one models, within this novel framework, was also performed to allow for early conclusions as to how well permafrost erosion can currently be modelled without more sophisticated setups. Article in Journal/Newspaper Arctic Arctic Climate change Ice permafrost Institut national de la recherche scientifique, Québec: Espace INRS Arctic Water 12 8 2254
institution Open Polar
collection Institut national de la recherche scientifique, Québec: Espace INRS
op_collection_id ftinrsquebec
language English
topic permafrost
erosion
coastal erosion
experimental modelling
spellingShingle permafrost
erosion
coastal erosion
experimental modelling
Korte, Sophia
Gieschen, Rebekka
Stolle, Jacob
Goseberg, Nils
Physical Modelling of Arctic Coastlines—Progress and Limitations.
topic_facet permafrost
erosion
coastal erosion
experimental modelling
description Permafrost coastlines represent a large portion of the world’s coastal area and these areas have become increasingly vulnerable in the face of climate change. The predominant mechanism of coastal erosion in these areas has been identified through several observational studies as thermomechanical erosion—a joint removal of sediment through the melting of interstitial ice (thermal energy) and abrasion from incoming waves (mechanical energy). However, further developments are needed looking how common design parameters in coastal engineering (such as wave height, period, sediment size, etc.) contribute to the process. This paper presents the current state of the art with the objective of establishing the necessary research background to develop a process-based approach to predicting permafrost erosion. To that end, an overarching framework is presented that includes all major, erosion-relevant processes, while delineating means to accomplish permafrost modelling in experimental studies. Preliminary modelling of generations zero and one models, within this novel framework, was also performed to allow for early conclusions as to how well permafrost erosion can currently be modelled without more sophisticated setups.
format Article in Journal/Newspaper
author Korte, Sophia
Gieschen, Rebekka
Stolle, Jacob
Goseberg, Nils
author_facet Korte, Sophia
Gieschen, Rebekka
Stolle, Jacob
Goseberg, Nils
author_sort Korte, Sophia
title Physical Modelling of Arctic Coastlines—Progress and Limitations.
title_short Physical Modelling of Arctic Coastlines—Progress and Limitations.
title_full Physical Modelling of Arctic Coastlines—Progress and Limitations.
title_fullStr Physical Modelling of Arctic Coastlines—Progress and Limitations.
title_full_unstemmed Physical Modelling of Arctic Coastlines—Progress and Limitations.
title_sort physical modelling of arctic coastlines—progress and limitations.
publishDate 2020
url https://espace.inrs.ca/id/eprint/10378/
https://espace.inrs.ca/id/eprint/10378/1/P3775.pdf
https://doi.org/10.3390/w12082254
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
Climate change
Ice
permafrost
genre_facet Arctic
Arctic
Climate change
Ice
permafrost
op_relation https://espace.inrs.ca/id/eprint/10378/1/P3775.pdf
Korte, Sophia, Gieschen, Rebekka, Stolle, Jacob orcid:0000-0003-0902-9339 et Goseberg, Nils (2020). Physical Modelling of Arctic Coastlines—Progress and Limitations. Water , vol. 12 , nº 8. p. 2254. DOI:10.3390/w12082254 <https://doi.org/10.3390/w12082254>.
doi:10.3390/w12082254
op_doi https://doi.org/10.3390/w12082254
container_title Water
container_volume 12
container_issue 8
container_start_page 2254
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