Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic

With observed increases in retrogressive thaw slump (RTS) number, rates, and size in recent decades, there is a need to understand these highly dynamic landforms as they impact surrounding ecosystems and infrastructure. There is a general lack of detailed (e.g., daily) field observations of change i...

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Main Authors: Ward Jones, Melissa K., Pollard, Wayne H.
Format: Article in Journal/Newspaper
Language:English
Published: The Arctic Institute of North America 2021
Subjects:
Online Access:https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377
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spelling ftunivcalgaryojs:oai:journalhosting.ucalgary.ca:article/73377 2023-05-15T14:19:02+02:00 Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic Ward Jones, Melissa K. Pollard, Wayne H. 2021-10-05 application/pdf https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377 eng eng The Arctic Institute of North America https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377/55192 https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377 Copyright (c) 2021 ARCTIC http://creativecommons.org/licenses/by/4.0/ CC-BY ARCTIC; Vol. 74 No. 3 (2021): SEPTEMBER: 239-417; 339-354 1923-1245 0004-0843 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion research-article 2021 ftunivcalgaryojs 2022-07-03T17:30:01Z With observed increases in retrogressive thaw slump (RTS) number, rates, and size in recent decades, there is a need to understand these highly dynamic landforms as they impact surrounding ecosystems and infrastructure. There is a general lack of detailed (e.g., daily) field observations of change in RTSs; we help fill this gap by monitoring three RTSs for much of the 2017 thaw period by setting up and tracking survey transects on a near daily basis. We correlated mean daily and cumulative retreat to mean daily air temperature (MDAT), total daily precipitation (TDP), and cumulative thawing degree days (TDD) using various polynomial regressions and Pearson correlation techniques. Our results show that July retreat was highly variable, and periods of increased RTS retreat did not always align with periods of increased air temperature. Also, multiple periods of increased retreat largely driven by sediment distribution in the RTS floor could occur within a single period of increased air temperature. Retreat rates decreased suddenly in early August, indicating a threshold of either air temperature, solar radiation or a combination of both must be reached for increased retreat rates. A statistically significant correlation was found between daily mean and mean cumulative retreat with MDAT (p > 0.001) and TDD (p > 0.001 and > 0.0001) but not with total daily precipitation. Correlating mean cumulative retreat and TDD using polynomial regression generated R2 values greater than 0.99 for all three sites. Both cumulative retreat and TDD account for past and current conditions, as well as lag responses, within the monitoring period. The high R2 values for the correlation of mean cumulative retreat and TDD suggest the potential for accurately modelling RTS retreat with minimal field data (air temperature and headwall position), however modelling is currently restricted to individual RTSs and only within short time scales. Monitoring RTSs on a daily scale allows RTS behaviour and trends to be identified that may be ... Article in Journal/Newspaper Arctic Arctic University of Calgary Journal Hosting Arctic
institution Open Polar
collection University of Calgary Journal Hosting
op_collection_id ftunivcalgaryojs
language English
description With observed increases in retrogressive thaw slump (RTS) number, rates, and size in recent decades, there is a need to understand these highly dynamic landforms as they impact surrounding ecosystems and infrastructure. There is a general lack of detailed (e.g., daily) field observations of change in RTSs; we help fill this gap by monitoring three RTSs for much of the 2017 thaw period by setting up and tracking survey transects on a near daily basis. We correlated mean daily and cumulative retreat to mean daily air temperature (MDAT), total daily precipitation (TDP), and cumulative thawing degree days (TDD) using various polynomial regressions and Pearson correlation techniques. Our results show that July retreat was highly variable, and periods of increased RTS retreat did not always align with periods of increased air temperature. Also, multiple periods of increased retreat largely driven by sediment distribution in the RTS floor could occur within a single period of increased air temperature. Retreat rates decreased suddenly in early August, indicating a threshold of either air temperature, solar radiation or a combination of both must be reached for increased retreat rates. A statistically significant correlation was found between daily mean and mean cumulative retreat with MDAT (p > 0.001) and TDD (p > 0.001 and > 0.0001) but not with total daily precipitation. Correlating mean cumulative retreat and TDD using polynomial regression generated R2 values greater than 0.99 for all three sites. Both cumulative retreat and TDD account for past and current conditions, as well as lag responses, within the monitoring period. The high R2 values for the correlation of mean cumulative retreat and TDD suggest the potential for accurately modelling RTS retreat with minimal field data (air temperature and headwall position), however modelling is currently restricted to individual RTSs and only within short time scales. Monitoring RTSs on a daily scale allows RTS behaviour and trends to be identified that may be ...
format Article in Journal/Newspaper
author Ward Jones, Melissa K.
Pollard, Wayne H.
spellingShingle Ward Jones, Melissa K.
Pollard, Wayne H.
Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
author_facet Ward Jones, Melissa K.
Pollard, Wayne H.
author_sort Ward Jones, Melissa K.
title Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
title_short Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
title_full Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
title_fullStr Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
title_full_unstemmed Daily Field Observations of Retrogressive Thaw Slump Dynamics in the Canadian High Arctic
title_sort daily field observations of retrogressive thaw slump dynamics in the canadian high arctic
publisher The Arctic Institute of North America
publishDate 2021
url https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377
geographic Arctic
geographic_facet Arctic
genre Arctic
Arctic
genre_facet Arctic
Arctic
op_source ARCTIC; Vol. 74 No. 3 (2021): SEPTEMBER: 239-417; 339-354
1923-1245
0004-0843
op_relation https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377/55192
https://journalhosting.ucalgary.ca/index.php/arctic/article/view/73377
op_rights Copyright (c) 2021 ARCTIC
http://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
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