Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...

In this study, we sampled lateral cross-sections of four relict ice wedges from retrogressive thaw slump and coastal bluf exposures on Hooper Island, Pelly Island, Richards Island and the mainland coast near Tuktoyaktuk. Ice blocks capturing the entire growth sequences of the ice wedges (i.e., ice w...

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Main Authors: Porter, Trevor, Holland, Kira, Buchanan, Casey, Froese, Duane, Kokelj, Steven
Format: Dataset
Language:unknown
Published: Canadian Cryospheric Information Network 2021
Subjects:
Online Access:https://dx.doi.org/10.21963/13163
https://www.polardata.ca/pdcsearch/?doi_id=13163
id ftdatacite:10.21963/13163
record_format openpolar
spelling ftdatacite:10.21963/13163 2024-09-15T18:02:20+00:00 Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ... Porter, Trevor Holland, Kira Buchanan, Casey Froese, Duane Kokelj, Steven 2021 https://dx.doi.org/10.21963/13163 https://www.polardata.ca/pdcsearch/?doi_id=13163 unknown Canadian Cryospheric Information Network Dataset dataset 2021 ftdatacite https://doi.org/10.21963/13163 2024-07-03T10:41:07Z In this study, we sampled lateral cross-sections of four relict ice wedges from retrogressive thaw slump and coastal bluf exposures on Hooper Island, Pelly Island, Richards Island and the mainland coast near Tuktoyaktuk. Ice blocks capturing the entire growth sequences of the ice wedges (i.e., ice wedge center to ice-sediment contact) were collected by chainsaw and kept frozen in field coolers, and later sub-sampled at high-resolution in a cold lab. The ice wedges were sub-sampled at 1-1.5 cm horizontal resolution, integrating ~1-3 ice veins per sample on average. We analysed the stable hydrogen- and oxygen-isotope ratios (δ2H and δ18O) of each sample (N = 803). The age of the ice was estimated by AMS-DO14C dating of 6 to 10 samples per ice wedge, evenly distributed across each wedge to capture the full range of ages. A composite δ18O record spanning the period 7,400-600 cal yr BP was also constructed using the dated samples only (N = 36). The all-sample co-isotope (δ2H-δ18O) data are defined by a regression ... : The ice wedge oxygen isotope data were collected to better understand long-term changes in the mean winter climate of the study region. Currently there are few data constraining changes in mean winter climate over the Holocene (last 11,700 years), but a relative abundance of data on the warm-summer season. The lack of winter data limits our ability to understand the sensitivity of the winter season to climate forcings such as insolation and greenhouse gas concentration, which is needed to better predict future climate change in the Arctic. These data contribute to a more holistic understanding of the Arctic climate system. ... Dataset Climate change Richards Island DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
description In this study, we sampled lateral cross-sections of four relict ice wedges from retrogressive thaw slump and coastal bluf exposures on Hooper Island, Pelly Island, Richards Island and the mainland coast near Tuktoyaktuk. Ice blocks capturing the entire growth sequences of the ice wedges (i.e., ice wedge center to ice-sediment contact) were collected by chainsaw and kept frozen in field coolers, and later sub-sampled at high-resolution in a cold lab. The ice wedges were sub-sampled at 1-1.5 cm horizontal resolution, integrating ~1-3 ice veins per sample on average. We analysed the stable hydrogen- and oxygen-isotope ratios (δ2H and δ18O) of each sample (N = 803). The age of the ice was estimated by AMS-DO14C dating of 6 to 10 samples per ice wedge, evenly distributed across each wedge to capture the full range of ages. A composite δ18O record spanning the period 7,400-600 cal yr BP was also constructed using the dated samples only (N = 36). The all-sample co-isotope (δ2H-δ18O) data are defined by a regression ... : The ice wedge oxygen isotope data were collected to better understand long-term changes in the mean winter climate of the study region. Currently there are few data constraining changes in mean winter climate over the Holocene (last 11,700 years), but a relative abundance of data on the warm-summer season. The lack of winter data limits our ability to understand the sensitivity of the winter season to climate forcings such as insolation and greenhouse gas concentration, which is needed to better predict future climate change in the Arctic. These data contribute to a more holistic understanding of the Arctic climate system. ...
format Dataset
author Porter, Trevor
Holland, Kira
Buchanan, Casey
Froese, Duane
Kokelj, Steven
spellingShingle Porter, Trevor
Holland, Kira
Buchanan, Casey
Froese, Duane
Kokelj, Steven
Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
author_facet Porter, Trevor
Holland, Kira
Buchanan, Casey
Froese, Duane
Kokelj, Steven
author_sort Porter, Trevor
title Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
title_short Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
title_full Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
title_fullStr Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
title_full_unstemmed Ice-wedge evidence of Holocene winter warming in the Canadian Arctic ...
title_sort ice-wedge evidence of holocene winter warming in the canadian arctic ...
publisher Canadian Cryospheric Information Network
publishDate 2021
url https://dx.doi.org/10.21963/13163
https://www.polardata.ca/pdcsearch/?doi_id=13163
genre Climate change
Richards Island
genre_facet Climate change
Richards Island
op_doi https://doi.org/10.21963/13163
_version_ 1810439802022002688