Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska
Ice-wedge polygons are widespread and conspicuous surficial expressions of ground-ice in permafrost landscapes. Thawing of ice wedges triggers differential ground subsidence, local ponding, and persistent changes to vegetation and hydrologic connectivity across the landscape. Here we characterize sp...
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ftdoajarticles:oai:doaj.org/article:5ab69278b8d142a0ab182754dcbc53e3 2023-05-15T14:54:11+02:00 Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska Gerald V. Frost Tracy Christopherson M. Torre Jorgenson Anna K. Liljedahl Matthew J. Macander Donald A. Walker Aaron F. Wells 2018-08-01T00:00:00Z https://doi.org/10.3390/rs10081312 https://doaj.org/article/5ab69278b8d142a0ab182754dcbc53e3 EN eng MDPI AG http://www.mdpi.com/2072-4292/10/8/1312 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10081312 https://doaj.org/article/5ab69278b8d142a0ab182754dcbc53e3 Remote Sensing, Vol 10, Iss 8, p 1312 (2018) permafrost ice wedge patterned ground thermokarst geomorphology Arctic tundra climate change North Slope Alaska Science Q article 2018 ftdoajarticles https://doi.org/10.3390/rs10081312 2022-12-31T07:30:20Z Ice-wedge polygons are widespread and conspicuous surficial expressions of ground-ice in permafrost landscapes. Thawing of ice wedges triggers differential ground subsidence, local ponding, and persistent changes to vegetation and hydrologic connectivity across the landscape. Here we characterize spatio-temporal patterns of ice-wedge degradation since circa 1950 across environmental gradients on Alaska’s North Slope. We used a spectral thresholding approach validated by field observations to map flooded thaw pits in high-resolution images from circa 1950, 1982, and 2012 for 11 study areas (1577–4460 ha). The total area of flooded pits increased since 1950 at 8 of 11 study areas (median change +3.6 ha; 130.3%). There were strong regional differences in the timing and extent of degradation; flooded pits were already extensive by 1950 on the Chukchi coastal plain (alluvial-marine deposits) and subsequent changes there indicate pit stabilization. Degradation began more recently on the central Beaufort coastal plain (eolian sand) and Arctic foothills (yedoma). Our results indicate that ice-wedge degradation in northern Alaska cannot be explained by late-20th century warmth alone. Likely mechanisms for asynchronous onset include landscape-scale differences in surficial materials and ground-ice content, regional climate gradients from west (maritime) to east (continental), and regional differences in the timing and magnitude of extreme warm summers after the Little Ice Age. Article in Journal/Newspaper Arctic Chukchi Climate change Ice north slope permafrost Thermokarst Tundra wedge* Alaska Directory of Open Access Journals: DOAJ Articles Arctic Remote Sensing 10 8 1312 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
permafrost ice wedge patterned ground thermokarst geomorphology Arctic tundra climate change North Slope Alaska Science Q |
spellingShingle |
permafrost ice wedge patterned ground thermokarst geomorphology Arctic tundra climate change North Slope Alaska Science Q Gerald V. Frost Tracy Christopherson M. Torre Jorgenson Anna K. Liljedahl Matthew J. Macander Donald A. Walker Aaron F. Wells Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
topic_facet |
permafrost ice wedge patterned ground thermokarst geomorphology Arctic tundra climate change North Slope Alaska Science Q |
description |
Ice-wedge polygons are widespread and conspicuous surficial expressions of ground-ice in permafrost landscapes. Thawing of ice wedges triggers differential ground subsidence, local ponding, and persistent changes to vegetation and hydrologic connectivity across the landscape. Here we characterize spatio-temporal patterns of ice-wedge degradation since circa 1950 across environmental gradients on Alaska’s North Slope. We used a spectral thresholding approach validated by field observations to map flooded thaw pits in high-resolution images from circa 1950, 1982, and 2012 for 11 study areas (1577–4460 ha). The total area of flooded pits increased since 1950 at 8 of 11 study areas (median change +3.6 ha; 130.3%). There were strong regional differences in the timing and extent of degradation; flooded pits were already extensive by 1950 on the Chukchi coastal plain (alluvial-marine deposits) and subsequent changes there indicate pit stabilization. Degradation began more recently on the central Beaufort coastal plain (eolian sand) and Arctic foothills (yedoma). Our results indicate that ice-wedge degradation in northern Alaska cannot be explained by late-20th century warmth alone. Likely mechanisms for asynchronous onset include landscape-scale differences in surficial materials and ground-ice content, regional climate gradients from west (maritime) to east (continental), and regional differences in the timing and magnitude of extreme warm summers after the Little Ice Age. |
format |
Article in Journal/Newspaper |
author |
Gerald V. Frost Tracy Christopherson M. Torre Jorgenson Anna K. Liljedahl Matthew J. Macander Donald A. Walker Aaron F. Wells |
author_facet |
Gerald V. Frost Tracy Christopherson M. Torre Jorgenson Anna K. Liljedahl Matthew J. Macander Donald A. Walker Aaron F. Wells |
author_sort |
Gerald V. Frost |
title |
Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
title_short |
Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
title_full |
Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
title_fullStr |
Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
title_full_unstemmed |
Regional Patterns and Asynchronous Onset of Ice-Wedge Degradation since the Mid-20th Century in Arctic Alaska |
title_sort |
regional patterns and asynchronous onset of ice-wedge degradation since the mid-20th century in arctic alaska |
publisher |
MDPI AG |
publishDate |
2018 |
url |
https://doi.org/10.3390/rs10081312 https://doaj.org/article/5ab69278b8d142a0ab182754dcbc53e3 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Chukchi Climate change Ice north slope permafrost Thermokarst Tundra wedge* Alaska |
genre_facet |
Arctic Chukchi Climate change Ice north slope permafrost Thermokarst Tundra wedge* Alaska |
op_source |
Remote Sensing, Vol 10, Iss 8, p 1312 (2018) |
op_relation |
http://www.mdpi.com/2072-4292/10/8/1312 https://doaj.org/toc/2072-4292 2072-4292 doi:10.3390/rs10081312 https://doaj.org/article/5ab69278b8d142a0ab182754dcbc53e3 |
op_doi |
https://doi.org/10.3390/rs10081312 |
container_title |
Remote Sensing |
container_volume |
10 |
container_issue |
8 |
container_start_page |
1312 |
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1766325906334285824 |