Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic

The fine-scale physical response of soils to thaw, ice content and soil water conditions in the High Arctic are poorly understood. This thesis introduces the topic and identifies knowledge gaps in the literature and secondly, addresses these gaps through the investigation of the spatiotemporal relat...

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Bibliographic Details
Main Author: Mcfadden, Sarah
Other Authors: Geography and Planning, Lamoureux, Scott
Format: Thesis
Language:English
Published: 2019
Subjects:
Ice
Online Access:http://hdl.handle.net/1974/26313
id ftqueensuniv:oai:https://qspace.library.queensu.ca:1974/26313
record_format openpolar
spelling ftqueensuniv:oai:https://qspace.library.queensu.ca:1974/26313 2024-06-02T08:01:02+00:00 Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic Mcfadden, Sarah Geography and Planning Lamoureux, Scott 2019-06-14T14:11:28Z application/pdf http://hdl.handle.net/1974/26313 eng eng Canadian theses http://hdl.handle.net/1974/26313 CC0 1.0 Universal Queen's University's Thesis/Dissertation Non-Exclusive License for Deposit to QSpace and Library and Archives Canada ProQuest PhD and Master's Theses International Dissemination Agreement Intellectual Property Guidelines at Queen's University Copying and Preserving Your Thesis This publication is made available by the authority of the copyright owner solely for the purpose of private study and research and may not be copied or reproduced except as permitted by the copyright laws without written authority from the copyright owner. http://creativecommons.org/publicdomain/zero/1.0/ permafrost Arctic soil water ground surface vertical displacement thesis 2019 ftqueensuniv 2024-05-06T10:47:32Z The fine-scale physical response of soils to thaw, ice content and soil water conditions in the High Arctic are poorly understood. This thesis introduces the topic and identifies knowledge gaps in the literature and secondly, addresses these gaps through the investigation of the spatiotemporal relationship between ground surface vertical displacement (GSVD) and active layer water level conditions during the summer thaw season at the Cape Bounty Arctic Watershed Observatory, Nunavut. GSVD and water level were monitored simultaneously at five measurement stations consisting of a new inclinometer system (accuracy ±0.15 mm) and a shallow subsurface well logged with pressure transducers. Diel cyclicity in both GSVD (± 0.5 mm) and water level (± 0.2 m) was present at two of the stations and synoptic scale variability characterized the others. The records indicate a close association between GSVD and water level at multiple short-term time scales. Active layer soil physics appear to be controlled by soil water content on both synoptic and diel timescales. Ground ice thaw appeared to be the primary source of water within the diel systems, while synoptic variability was associated with rainfall events. The diel systems were inferred to be primarily driven by large-scale (>258 m2) upslope contributing areas which facilitated diel water level and GSVD fluctuations due to the amplification of thaw-derived water accumulation downslope. These results improve our knowledge of the physical response of High Arctic soils to changes in soil water conditions and active layer thaw, critical for future landscape stability monitoring and geohazard prediction. M.Sc. Thesis Arctic Ice Nunavut permafrost Queen's University, Ontario: QSpace Arctic Nunavut Cape Bounty ENVELOPE(-109.542,-109.542,74.863,74.863)
institution Open Polar
collection Queen's University, Ontario: QSpace
op_collection_id ftqueensuniv
language English
topic permafrost
Arctic
soil water
ground surface vertical displacement
spellingShingle permafrost
Arctic
soil water
ground surface vertical displacement
Mcfadden, Sarah
Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
topic_facet permafrost
Arctic
soil water
ground surface vertical displacement
description The fine-scale physical response of soils to thaw, ice content and soil water conditions in the High Arctic are poorly understood. This thesis introduces the topic and identifies knowledge gaps in the literature and secondly, addresses these gaps through the investigation of the spatiotemporal relationship between ground surface vertical displacement (GSVD) and active layer water level conditions during the summer thaw season at the Cape Bounty Arctic Watershed Observatory, Nunavut. GSVD and water level were monitored simultaneously at five measurement stations consisting of a new inclinometer system (accuracy ±0.15 mm) and a shallow subsurface well logged with pressure transducers. Diel cyclicity in both GSVD (± 0.5 mm) and water level (± 0.2 m) was present at two of the stations and synoptic scale variability characterized the others. The records indicate a close association between GSVD and water level at multiple short-term time scales. Active layer soil physics appear to be controlled by soil water content on both synoptic and diel timescales. Ground ice thaw appeared to be the primary source of water within the diel systems, while synoptic variability was associated with rainfall events. The diel systems were inferred to be primarily driven by large-scale (>258 m2) upslope contributing areas which facilitated diel water level and GSVD fluctuations due to the amplification of thaw-derived water accumulation downslope. These results improve our knowledge of the physical response of High Arctic soils to changes in soil water conditions and active layer thaw, critical for future landscape stability monitoring and geohazard prediction. M.Sc.
author2 Geography and Planning
Lamoureux, Scott
format Thesis
author Mcfadden, Sarah
author_facet Mcfadden, Sarah
author_sort Mcfadden, Sarah
title Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
title_short Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
title_full Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
title_fullStr Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
title_full_unstemmed Fine-Scale Ground Surface Vertical Displacement and Soil Water Processes in the Canadian High Arctic
title_sort fine-scale ground surface vertical displacement and soil water processes in the canadian high arctic
publishDate 2019
url http://hdl.handle.net/1974/26313
long_lat ENVELOPE(-109.542,-109.542,74.863,74.863)
geographic Arctic
Nunavut
Cape Bounty
geographic_facet Arctic
Nunavut
Cape Bounty
genre Arctic
Ice
Nunavut
permafrost
genre_facet Arctic
Ice
Nunavut
permafrost
op_relation Canadian theses
http://hdl.handle.net/1974/26313
op_rights CC0 1.0 Universal
Queen's University's Thesis/Dissertation Non-Exclusive License for Deposit to QSpace and Library and Archives Canada
ProQuest PhD and Master's Theses International Dissemination Agreement
Intellectual Property Guidelines at Queen's University
Copying and Preserving Your Thesis
This publication is made available by the authority of the copyright owner solely for the purpose of private study and research and may not be copied or reproduced except as permitted by the copyright laws without written authority from the copyright owner.
http://creativecommons.org/publicdomain/zero/1.0/
_version_ 1800745276637446144