Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks
The intensification of thaw-driven mass wasting is transforming glacially conditioned permafrost terrain, coupling slopes with aquatic systems, and triggering a cascade of downstream effects. Within the context of recent, rapidly evolving climate controls on the geomorphology of permafrost terrain,...
Published in: | The Cryosphere |
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Copernicus Publications
2021
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Online Access: | https://doi.org/10.5194/tc-15-3059-2021 https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:6c8c1d9d6e344c6dbc65166424db58db 2023-05-15T15:15:45+02:00 Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks S. V. Kokelj J. Kokoszka J. van der Sluijs A. C. A. Rudy J. Tunnicliffe S. Shakil S. E. Tank S. Zolkos 2021-07-01 https://doi.org/10.5194/tc-15-3059-2021 https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db en eng Copernicus Publications doi:10.5194/tc-15-3059-2021 1994-0416 1994-0424 https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db undefined The Cryosphere, Vol 15, Pp 3059-3081 (2021) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple https://doi.org/10.5194/tc-15-3059-2021 2023-01-22T18:11:37Z The intensification of thaw-driven mass wasting is transforming glacially conditioned permafrost terrain, coupling slopes with aquatic systems, and triggering a cascade of downstream effects. Within the context of recent, rapidly evolving climate controls on the geomorphology of permafrost terrain, we (A) quantify three-dimensional retrogressive thaw slump enlargement and describe the processes and thresholds coupling slopes to downstream systems, (B) investigate catchment-scale patterns of slope thermokarst impacts and the geomorphic implications, and (C) map the propagation of effects through hydrological networks draining permafrost terrain of northwestern Canada. Power-law relationships between retrogressive thaw slump area and volume (R2=0.90), as well as the thickness of permafrost thawed (R2=0.63), combined with the multi-decadal (1986–2018) increase in the areal extent of thaw slump disturbance, show a 2 order of magnitude increase in catchment-scale geomorphic activity and the coupling of slope and hydrological systems. Predominant effects are to first- and second-order streams where sediment delivery, often indicated by formation of recent debris tongue deposits, commonly exceeds the transport capacity of headwater streams by orders of magnitude, signaling centennial- to millennial-scale perturbation of downstream systems. Assessment of hydrological networks indicates that thaw-driven mass wasting directly affects over 5538 km of stream segments, 889 km of coastline, and 1379 lakes in the 994 860 km2 study area. Downstream propagation of slope thermokarst indicates a potential increase in the number of affected lakes by at least a factor of 4 (n>5692) and impacted stream length by a factor of 8 (>44 343 km), and it defines several major impact zones on lakes, deltas, and coastal areas. Prince of Wales Strait is the receiving marine environment for greatly increased sediment and geochemical fluxes from numerous slump-impacted hydrological networks draining Banks Island and Victoria Island. The ... Article in Journal/Newspaper Arctic Banks Island permafrost Prince of Wales Strait The Cryosphere Thermokarst Victoria Island victoria island Unknown Arctic Canada Prince of Wales Strait ENVELOPE(-118.324,-118.324,72.706,72.706) The Cryosphere 15 7 3059 3081 |
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Open Polar |
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Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
geo envir |
spellingShingle |
geo envir S. V. Kokelj J. Kokoszka J. van der Sluijs A. C. A. Rudy J. Tunnicliffe S. Shakil S. E. Tank S. Zolkos Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
topic_facet |
geo envir |
description |
The intensification of thaw-driven mass wasting is transforming glacially conditioned permafrost terrain, coupling slopes with aquatic systems, and triggering a cascade of downstream effects. Within the context of recent, rapidly evolving climate controls on the geomorphology of permafrost terrain, we (A) quantify three-dimensional retrogressive thaw slump enlargement and describe the processes and thresholds coupling slopes to downstream systems, (B) investigate catchment-scale patterns of slope thermokarst impacts and the geomorphic implications, and (C) map the propagation of effects through hydrological networks draining permafrost terrain of northwestern Canada. Power-law relationships between retrogressive thaw slump area and volume (R2=0.90), as well as the thickness of permafrost thawed (R2=0.63), combined with the multi-decadal (1986–2018) increase in the areal extent of thaw slump disturbance, show a 2 order of magnitude increase in catchment-scale geomorphic activity and the coupling of slope and hydrological systems. Predominant effects are to first- and second-order streams where sediment delivery, often indicated by formation of recent debris tongue deposits, commonly exceeds the transport capacity of headwater streams by orders of magnitude, signaling centennial- to millennial-scale perturbation of downstream systems. Assessment of hydrological networks indicates that thaw-driven mass wasting directly affects over 5538 km of stream segments, 889 km of coastline, and 1379 lakes in the 994 860 km2 study area. Downstream propagation of slope thermokarst indicates a potential increase in the number of affected lakes by at least a factor of 4 (n>5692) and impacted stream length by a factor of 8 (>44 343 km), and it defines several major impact zones on lakes, deltas, and coastal areas. Prince of Wales Strait is the receiving marine environment for greatly increased sediment and geochemical fluxes from numerous slump-impacted hydrological networks draining Banks Island and Victoria Island. The ... |
format |
Article in Journal/Newspaper |
author |
S. V. Kokelj J. Kokoszka J. van der Sluijs A. C. A. Rudy J. Tunnicliffe S. Shakil S. E. Tank S. Zolkos |
author_facet |
S. V. Kokelj J. Kokoszka J. van der Sluijs A. C. A. Rudy J. Tunnicliffe S. Shakil S. E. Tank S. Zolkos |
author_sort |
S. V. Kokelj |
title |
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
title_short |
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
title_full |
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
title_fullStr |
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
title_full_unstemmed |
Thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through Arctic drainage networks |
title_sort |
thaw-driven mass wasting couples slopes with downstream systems, and effects propagate through arctic drainage networks |
publisher |
Copernicus Publications |
publishDate |
2021 |
url |
https://doi.org/10.5194/tc-15-3059-2021 https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db |
long_lat |
ENVELOPE(-118.324,-118.324,72.706,72.706) |
geographic |
Arctic Canada Prince of Wales Strait |
geographic_facet |
Arctic Canada Prince of Wales Strait |
genre |
Arctic Banks Island permafrost Prince of Wales Strait The Cryosphere Thermokarst Victoria Island victoria island |
genre_facet |
Arctic Banks Island permafrost Prince of Wales Strait The Cryosphere Thermokarst Victoria Island victoria island |
op_source |
The Cryosphere, Vol 15, Pp 3059-3081 (2021) |
op_relation |
doi:10.5194/tc-15-3059-2021 1994-0416 1994-0424 https://tc.copernicus.org/articles/15/3059/2021/tc-15-3059-2021.pdf https://doaj.org/article/6c8c1d9d6e344c6dbc65166424db58db |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-15-3059-2021 |
container_title |
The Cryosphere |
container_volume |
15 |
container_issue |
7 |
container_start_page |
3059 |
op_container_end_page |
3081 |
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1766346093005635584 |