Patterns of Discontinuous Permafrost Thaw in Peatlands

Climate warming in discontinuous permafrost peatlands is causing permafrost loss and changes in ecosystem dynamics at an unprecedented rate. Though rates of permafrost loss and landscape change have been widely documented based on remote sensing and field measurements, the local mechanisms of permaf...

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Main Authors: Devoie, Élise, Quinton, William L.
Format: Other/Unknown Material
Language:English
Published: Borealis 2020
Subjects:
Online Access:https://doi.org/10.5683/SP2/J2KBPF
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spelling ftborealisdata:doi:10.5683/SP2/J2KBPF 2023-05-15T16:17:53+02:00 Patterns of Discontinuous Permafrost Thaw in Peatlands Devoie, Élise Quinton, William L. Devoie, Élise 2020-01-01 https://doi.org/10.5683/SP2/J2KBPF English eng Borealis Devoie, Élise; Quinton, William L, 2021, "Data for: Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes", https://doi.org/10.5683/SP2/YR6TQ8, Scholars Portal Dataverse. Quinton, William L.; Connon, Ryan F.; Devoie, Élise G., 2019, "Permafrost Monitoring at Scotty Creek Research Station, 2011-2017 [Northwest Territories, Canada]", https://doi.org/10.5683/SP2/BTRLHO, Scholars Portal Dataverse. Haynes, Kristine M.; Connon, Ryan F.; Quinton, William L., 2018, "Hydrometeorological measurements in peatland-dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada", https://doi.org/10.5683/SP/OQDRJG, Scholars Portal Dataverse. Quinton, William; Connon, Ryan; Devoie, Élise; Hayashi, Masaki; Veness, Tyler, 2018, "Micrometeorological and freeze-thaw data at Scotty Creek, NT 2001-2017 [Canada]", https://doi.org/10.5683/SP/EMDB8K, Scholars Portal Dataverse. https://doi.org/10.5683/SP2/J2KBPF Earth and Environmental Sciences permafrost meteorological timeseries data 2020 ftborealisdata https://doi.org/10.5683/SP2/J2KBPF https://doi.org/10.5683/SP2/YR6TQ8 https://doi.org/10.5683/SP2/BTRLHO https://doi.org/10.5683/SP/OQDRJG https://doi.org/10.5683/SP/EMDB8K 2022-10-10T05:31:06Z Climate warming in discontinuous permafrost peatlands is causing permafrost loss and changes in ecosystem dynamics at an unprecedented rate. Though rates of permafrost loss and landscape change have been widely documented based on remote sensing and field measurements, the local mechanisms of permafrost degradation remain under-studied. Data collected over three decades of research in the Scotty Creek study basin in the southern Northwest Territories of Canada was analyzed to find vertical conduction accounts for most vertical permafrost degradation, while advective processes are needed to describe thaw in features which are subject to seasonal flows. It was found that heat advection was necessary to describe lateral thaw rates, which are up to an order of magnitude greater than vertical thaw. Thaw from below, driven either by the geothermal gradient or groundwater flow, may account for up to 10 cm of permafrost thaw annually. Once these thaw mechanisms were established, the hydrologic, thermodynamic and geophysical function of taliks in different parts of the landscape were considered in light of the data collected at the and surrounding area. This analysis is supported through the use of ERT data detailing the subsurface permafrost structure. Data collected at Scotty Creek points to a pattern of talik evolution and permafrost degradation. This understanding of local thaw mechanisms and trajectory is an important first step in being able to predict distributed permafrost thaw in peatlands. This research data is associated with Scotty Creek Research Station, 50km south of Fort Simpson, in the Northwest Territories, Canada. Learn more about SCRS and its research at http://scottycreek.com . Other/Unknown Material Fort Simpson Northwest Territories permafrost Borealis Canada Fort Simpson ENVELOPE(-121.320,-121.320,61.808,61.808) Northwest Territories Scotty Creek ENVELOPE(-121.561,-121.561,61.436,61.436) Talik ENVELOPE(146.601,146.601,59.667,59.667)
institution Open Polar
collection Borealis
op_collection_id ftborealisdata
language English
topic Earth and Environmental Sciences
permafrost
spellingShingle Earth and Environmental Sciences
permafrost
Devoie, Élise
Quinton, William L.
Patterns of Discontinuous Permafrost Thaw in Peatlands
topic_facet Earth and Environmental Sciences
permafrost
description Climate warming in discontinuous permafrost peatlands is causing permafrost loss and changes in ecosystem dynamics at an unprecedented rate. Though rates of permafrost loss and landscape change have been widely documented based on remote sensing and field measurements, the local mechanisms of permafrost degradation remain under-studied. Data collected over three decades of research in the Scotty Creek study basin in the southern Northwest Territories of Canada was analyzed to find vertical conduction accounts for most vertical permafrost degradation, while advective processes are needed to describe thaw in features which are subject to seasonal flows. It was found that heat advection was necessary to describe lateral thaw rates, which are up to an order of magnitude greater than vertical thaw. Thaw from below, driven either by the geothermal gradient or groundwater flow, may account for up to 10 cm of permafrost thaw annually. Once these thaw mechanisms were established, the hydrologic, thermodynamic and geophysical function of taliks in different parts of the landscape were considered in light of the data collected at the and surrounding area. This analysis is supported through the use of ERT data detailing the subsurface permafrost structure. Data collected at Scotty Creek points to a pattern of talik evolution and permafrost degradation. This understanding of local thaw mechanisms and trajectory is an important first step in being able to predict distributed permafrost thaw in peatlands. This research data is associated with Scotty Creek Research Station, 50km south of Fort Simpson, in the Northwest Territories, Canada. Learn more about SCRS and its research at http://scottycreek.com .
author2 Devoie, Élise
format Other/Unknown Material
author Devoie, Élise
Quinton, William L.
author_facet Devoie, Élise
Quinton, William L.
author_sort Devoie, Élise
title Patterns of Discontinuous Permafrost Thaw in Peatlands
title_short Patterns of Discontinuous Permafrost Thaw in Peatlands
title_full Patterns of Discontinuous Permafrost Thaw in Peatlands
title_fullStr Patterns of Discontinuous Permafrost Thaw in Peatlands
title_full_unstemmed Patterns of Discontinuous Permafrost Thaw in Peatlands
title_sort patterns of discontinuous permafrost thaw in peatlands
publisher Borealis
publishDate 2020
url https://doi.org/10.5683/SP2/J2KBPF
long_lat ENVELOPE(-121.320,-121.320,61.808,61.808)
ENVELOPE(-121.561,-121.561,61.436,61.436)
ENVELOPE(146.601,146.601,59.667,59.667)
geographic Canada
Fort Simpson
Northwest Territories
Scotty Creek
Talik
geographic_facet Canada
Fort Simpson
Northwest Territories
Scotty Creek
Talik
genre Fort Simpson
Northwest Territories
permafrost
genre_facet Fort Simpson
Northwest Territories
permafrost
op_relation Devoie, Élise; Quinton, William L, 2021, "Data for: Subsurface flow measurements using passive flux meters in variably‐saturated cold‐regions landscapes", https://doi.org/10.5683/SP2/YR6TQ8, Scholars Portal Dataverse.
Quinton, William L.; Connon, Ryan F.; Devoie, Élise G., 2019, "Permafrost Monitoring at Scotty Creek Research Station, 2011-2017 [Northwest Territories, Canada]", https://doi.org/10.5683/SP2/BTRLHO, Scholars Portal Dataverse.
Haynes, Kristine M.; Connon, Ryan F.; Quinton, William L., 2018, "Hydrometeorological measurements in peatland-dominated, discontinuous permafrost at Scotty Creek, Northwest Territories, Canada", https://doi.org/10.5683/SP/OQDRJG, Scholars Portal Dataverse.
Quinton, William; Connon, Ryan; Devoie, Élise; Hayashi, Masaki; Veness, Tyler, 2018, "Micrometeorological and freeze-thaw data at Scotty Creek, NT 2001-2017 [Canada]", https://doi.org/10.5683/SP/EMDB8K, Scholars Portal Dataverse.
https://doi.org/10.5683/SP2/J2KBPF
op_doi https://doi.org/10.5683/SP2/J2KBPF
https://doi.org/10.5683/SP2/YR6TQ8
https://doi.org/10.5683/SP2/BTRLHO
https://doi.org/10.5683/SP/OQDRJG
https://doi.org/10.5683/SP/EMDB8K
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