Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada

The southern Beaufort coastline in Canada experiences significant storm surge events that are thought to play an important role in coastal erosion and influence permafrost dynamics. Unfortunately, many of these events have not been documented with tide gauge records. In this paper, we evaluate coast...

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Published in:Frontiers in Earth Science
Main Authors: Roger F. MacLeod, Scott R. Dallimore
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2021
Subjects:
Q
Online Access:https://doi.org/10.3389/feart.2021.698660
https://doaj.org/article/a70aa0eb6d2e48bf9f84e2bf89a81520
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spelling ftdoajarticles:oai:doaj.org/article:a70aa0eb6d2e48bf9f84e2bf89a81520 2023-05-15T15:03:41+02:00 Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada Roger F. MacLeod Scott R. Dallimore 2021-12-01T00:00:00Z https://doi.org/10.3389/feart.2021.698660 https://doaj.org/article/a70aa0eb6d2e48bf9f84e2bf89a81520 EN eng Frontiers Media S.A. https://www.frontiersin.org/articles/10.3389/feart.2021.698660/full https://doaj.org/toc/2296-6463 2296-6463 doi:10.3389/feart.2021.698660 https://doaj.org/article/a70aa0eb6d2e48bf9f84e2bf89a81520 Frontiers in Earth Science, Vol 9 (2021) storm surge coastal erosion structure from motion coastal hazards arctic storms unoccupied aerial vehicle Science Q article 2021 ftdoajarticles https://doi.org/10.3389/feart.2021.698660 2022-12-31T11:52:40Z The southern Beaufort coastline in Canada experiences significant storm surge events that are thought to play an important role in coastal erosion and influence permafrost dynamics. Unfortunately, many of these events have not been documented with tide gauge records. In this paper, we evaluate coastal driftwood accumulations as a proxy for estimating maximum storm surge heights and the history of these events. We use historical air photos and data derived from Unoccupied Aerial Vehicle (UAV) imagery to resurvey four coastal stranded driftwood study sites that were first appraised in 1985–86 and assess two new regional sites in the Mackenzie Delta. Maximum storm surge heights were found to be similar to observations carried out in the 1980s, however, we refine the elevations with more accuracy and reference these to a vertical datum appropriate for incorporating into sea level hazard assessments. Detailed mapping, historical air photo comparisons and the UAV acquired imagery at a site close to Tuktoyaktuk demonstrate that the highest storm surge at this site (1.98 m CGVD2013) occurred in association with a severe storm in 1970. This event shifted driftwood and floated material slightly upslope from an older event thought to occur in 1944 that reached 1.85 m (CGVD2013) elevation. The quality and accuracy of the high-resolution Digital Surface Model (DSM) and orthophoto derived from Structure from Motion (SfM) processing of the UAV photographs allowed mapping of four distinct stratigraphic units within the driftwood piles. Based on variations in anthropogenic debris composition, weathering characteristics and history of movement on aerial photographs, we conclude that no storm surge events at Tuktoyaktuk have exceeded ∼1.3 m (CGVD2013) since 1970. While there has been some speculation that ongoing climate change may lead to more frequent large magnitude storm surges along the Beaufort coast, our study and available tide gauge measurements, suggest that while moderate elevation storm surges may be more frequent in ... Article in Journal/Newspaper Arctic Climate change Mackenzie Delta permafrost Directory of Open Access Journals: DOAJ Articles Arctic Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833) Tuktoyaktuk ENVELOPE(-133.006,-133.006,69.425,69.425) Frontiers in Earth Science 9
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic storm surge
coastal erosion
structure from motion
coastal hazards
arctic storms
unoccupied aerial vehicle
Science
Q
spellingShingle storm surge
coastal erosion
structure from motion
coastal hazards
arctic storms
unoccupied aerial vehicle
Science
Q
Roger F. MacLeod
Scott R. Dallimore
Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
topic_facet storm surge
coastal erosion
structure from motion
coastal hazards
arctic storms
unoccupied aerial vehicle
Science
Q
description The southern Beaufort coastline in Canada experiences significant storm surge events that are thought to play an important role in coastal erosion and influence permafrost dynamics. Unfortunately, many of these events have not been documented with tide gauge records. In this paper, we evaluate coastal driftwood accumulations as a proxy for estimating maximum storm surge heights and the history of these events. We use historical air photos and data derived from Unoccupied Aerial Vehicle (UAV) imagery to resurvey four coastal stranded driftwood study sites that were first appraised in 1985–86 and assess two new regional sites in the Mackenzie Delta. Maximum storm surge heights were found to be similar to observations carried out in the 1980s, however, we refine the elevations with more accuracy and reference these to a vertical datum appropriate for incorporating into sea level hazard assessments. Detailed mapping, historical air photo comparisons and the UAV acquired imagery at a site close to Tuktoyaktuk demonstrate that the highest storm surge at this site (1.98 m CGVD2013) occurred in association with a severe storm in 1970. This event shifted driftwood and floated material slightly upslope from an older event thought to occur in 1944 that reached 1.85 m (CGVD2013) elevation. The quality and accuracy of the high-resolution Digital Surface Model (DSM) and orthophoto derived from Structure from Motion (SfM) processing of the UAV photographs allowed mapping of four distinct stratigraphic units within the driftwood piles. Based on variations in anthropogenic debris composition, weathering characteristics and history of movement on aerial photographs, we conclude that no storm surge events at Tuktoyaktuk have exceeded ∼1.3 m (CGVD2013) since 1970. While there has been some speculation that ongoing climate change may lead to more frequent large magnitude storm surges along the Beaufort coast, our study and available tide gauge measurements, suggest that while moderate elevation storm surges may be more frequent in ...
format Article in Journal/Newspaper
author Roger F. MacLeod
Scott R. Dallimore
author_facet Roger F. MacLeod
Scott R. Dallimore
author_sort Roger F. MacLeod
title Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
title_short Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
title_full Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
title_fullStr Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
title_full_unstemmed Assessment of Storm Surge History as Recorded by Driftwood in the Mackenzie Delta and Tuktoyaktuk Coastlands, Arctic Canada
title_sort assessment of storm surge history as recorded by driftwood in the mackenzie delta and tuktoyaktuk coastlands, arctic canada
publisher Frontiers Media S.A.
publishDate 2021
url https://doi.org/10.3389/feart.2021.698660
https://doaj.org/article/a70aa0eb6d2e48bf9f84e2bf89a81520
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
ENVELOPE(-133.006,-133.006,69.425,69.425)
geographic Arctic
Canada
Mackenzie Delta
Tuktoyaktuk
geographic_facet Arctic
Canada
Mackenzie Delta
Tuktoyaktuk
genre Arctic
Climate change
Mackenzie Delta
permafrost
genre_facet Arctic
Climate change
Mackenzie Delta
permafrost
op_source Frontiers in Earth Science, Vol 9 (2021)
op_relation https://www.frontiersin.org/articles/10.3389/feart.2021.698660/full
https://doaj.org/toc/2296-6463
2296-6463
doi:10.3389/feart.2021.698660
https://doaj.org/article/a70aa0eb6d2e48bf9f84e2bf89a81520
op_doi https://doi.org/10.3389/feart.2021.698660
container_title Frontiers in Earth Science
container_volume 9
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