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: Sophia Korte, Rebekka Gieschen, Jacob Stolle, Nils Goseberg
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2020
Subjects:
Ice
Online Access:https://doi.org/10.3390/w12082254
https://doaj.org/article/092215b1ade440c5917becc834dfbafa
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spelling ftdoajarticles:oai:doaj.org/article:092215b1ade440c5917becc834dfbafa 2023-05-15T15:06:04+02:00 Physical Modelling of Arctic Coastlines—Progress and Limitations Sophia Korte Rebekka Gieschen Jacob Stolle Nils Goseberg 2020-08-01T00:00:00Z https://doi.org/10.3390/w12082254 https://doaj.org/article/092215b1ade440c5917becc834dfbafa EN eng MDPI AG https://www.mdpi.com/2073-4441/12/8/2254 https://doaj.org/toc/2073-4441 doi:10.3390/w12082254 2073-4441 https://doaj.org/article/092215b1ade440c5917becc834dfbafa Water, Vol 12, Iss 2254, p 2254 (2020) permafrost erosion coastal erosion experimental modelling Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 article 2020 ftdoajarticles https://doi.org/10.3390/w12082254 2022-12-31T09:46:49Z 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 Climate change Ice permafrost Directory of Open Access Journals: DOAJ Articles Arctic Water 12 8 2254
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic permafrost
erosion
coastal erosion
experimental modelling
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle permafrost
erosion
coastal erosion
experimental modelling
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Sophia Korte
Rebekka Gieschen
Jacob Stolle
Nils Goseberg
Physical Modelling of Arctic Coastlines—Progress and Limitations
topic_facet permafrost
erosion
coastal erosion
experimental modelling
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
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 Sophia Korte
Rebekka Gieschen
Jacob Stolle
Nils Goseberg
author_facet Sophia Korte
Rebekka Gieschen
Jacob Stolle
Nils Goseberg
author_sort Sophia Korte
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
publisher MDPI AG
publishDate 2020
url https://doi.org/10.3390/w12082254
https://doaj.org/article/092215b1ade440c5917becc834dfbafa
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Ice
permafrost
genre_facet Arctic
Climate change
Ice
permafrost
op_source Water, Vol 12, Iss 2254, p 2254 (2020)
op_relation https://www.mdpi.com/2073-4441/12/8/2254
https://doaj.org/toc/2073-4441
doi:10.3390/w12082254
2073-4441
https://doaj.org/article/092215b1ade440c5917becc834dfbafa
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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