Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes

Yukon’s Beaufort coast, Canada, is a highly dynamic landscape. Cultural sites, infrastructure, and travel routes used by the local population are particularly vulnerable to coastal erosion. To assess threats to these phenomena, rates of shoreline change for a 210km length of the coast were analyzed...

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Published in:Arctic Science
Main Authors: Irrgang, Anna M., Lantuit, Hugues, Gordon, Richard R., Piskor, Ashley, Manson, Gavin K.
Format: Article in Journal/Newspaper
Language:English
Published: Zenodo 2019
Subjects:
Online Access:https://doi.org/10.1139/as-2017-0041
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spelling ftzenodo:oai:zenodo.org:2633810 2024-09-15T18:15:10+00:00 Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes Irrgang, Anna M. Lantuit, Hugues Gordon, Richard R. Piskor, Ashley Manson, Gavin K. 2019-02-11 https://doi.org/10.1139/as-2017-0041 eng eng Zenodo https://zenodo.org/communities/nunataryuk https://doi.org/10.1139/as-2017-0041 oai:zenodo.org:2633810 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Arctic coastal dynamics permafrost coast shoreline projection Inuvialuit cultural features info:eu-repo/semantics/article 2019 ftzenodo https://doi.org/10.1139/as-2017-0041 2024-07-25T20:31:04Z Yukon’s Beaufort coast, Canada, is a highly dynamic landscape. Cultural sites, infrastructure, and travel routes used by the local population are particularly vulnerable to coastal erosion. To assess threats to these phenomena, rates of shoreline change for a 210km length of the coast were analyzed and combined with socioeconomic and cultural information. Rates of shoreline change were derived from aerial and satellite imagery from the 1950s, 1970s, 1990s, and 2011. Using these data, conservative (S1) and dynamic (S2) shoreline projections were constructed to predict shoreline positions for the year 2100. The locations of cultural features in the archives of a Parks Canada database, the Yukon Archaeological Program, and as reported in other literature were combined with projected shoreline position changes. Between 2011 and 2100, approximately 850ha (S1) and 2660ha (S2) may erode, resulting in a loss of 45% (S1) to 61% (S2) of all cultural features by 2100. The last large, actively used camp area and two nearshore landing strips will likely be threatened by future coastal processes. Future coastal erosion and sedimentation processes are expected to increasingly threaten cultural sites and influence travelling and living along the Yukon coast. Article in Journal/Newspaper Inuvialuit permafrost Yukon Zenodo Arctic Science 5 2 107 126
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Arctic coastal dynamics
permafrost coast
shoreline projection
Inuvialuit cultural features
spellingShingle Arctic coastal dynamics
permafrost coast
shoreline projection
Inuvialuit cultural features
Irrgang, Anna M.
Lantuit, Hugues
Gordon, Richard R.
Piskor, Ashley
Manson, Gavin K.
Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
topic_facet Arctic coastal dynamics
permafrost coast
shoreline projection
Inuvialuit cultural features
description Yukon’s Beaufort coast, Canada, is a highly dynamic landscape. Cultural sites, infrastructure, and travel routes used by the local population are particularly vulnerable to coastal erosion. To assess threats to these phenomena, rates of shoreline change for a 210km length of the coast were analyzed and combined with socioeconomic and cultural information. Rates of shoreline change were derived from aerial and satellite imagery from the 1950s, 1970s, 1990s, and 2011. Using these data, conservative (S1) and dynamic (S2) shoreline projections were constructed to predict shoreline positions for the year 2100. The locations of cultural features in the archives of a Parks Canada database, the Yukon Archaeological Program, and as reported in other literature were combined with projected shoreline position changes. Between 2011 and 2100, approximately 850ha (S1) and 2660ha (S2) may erode, resulting in a loss of 45% (S1) to 61% (S2) of all cultural features by 2100. The last large, actively used camp area and two nearshore landing strips will likely be threatened by future coastal processes. Future coastal erosion and sedimentation processes are expected to increasingly threaten cultural sites and influence travelling and living along the Yukon coast.
format Article in Journal/Newspaper
author Irrgang, Anna M.
Lantuit, Hugues
Gordon, Richard R.
Piskor, Ashley
Manson, Gavin K.
author_facet Irrgang, Anna M.
Lantuit, Hugues
Gordon, Richard R.
Piskor, Ashley
Manson, Gavin K.
author_sort Irrgang, Anna M.
title Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
title_short Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
title_full Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
title_fullStr Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
title_full_unstemmed Impacts of past and future coastal changes on the Yukon coast — threats for cultural sites, infrastructure, and travel routes
title_sort impacts of past and future coastal changes on the yukon coast — threats for cultural sites, infrastructure, and travel routes
publisher Zenodo
publishDate 2019
url https://doi.org/10.1139/as-2017-0041
genre Inuvialuit
permafrost
Yukon
genre_facet Inuvialuit
permafrost
Yukon
op_relation https://zenodo.org/communities/nunataryuk
https://doi.org/10.1139/as-2017-0041
oai:zenodo.org:2633810
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1139/as-2017-0041
container_title Arctic Science
container_volume 5
container_issue 2
container_start_page 107
op_container_end_page 126
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