Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum
Local glaciers and ice caps ( GIC s) comprise only ~5.4% of the total ice volume, but account for ~14–20% of the current ice loss in Greenland. The glacial history of GIC s is not well constrained, however, and little is known about how they reacted to Holocene climate changes. Specifically, in Nort...
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crwiley:10.1111/bor.12384 2024-06-02T08:02:39+00:00 Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum Larsen, Nicolaj K. Levy, Laura B. Strunk, Astrid Søndergaard, Anne Sofie Olsen, Jesper Lauridsen, Torben L. Arctic Research Centre Aarhus University Villum Young Investigator Programme 2019 http://dx.doi.org/10.1111/bor.12384 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12384 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12384 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12384 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Boreas volume 48, issue 3, page 551-562 ISSN 0300-9483 1502-3885 journal-article 2019 crwiley https://doi.org/10.1111/bor.12384 2024-05-03T12:02:25Z Local glaciers and ice caps ( GIC s) comprise only ~5.4% of the total ice volume, but account for ~14–20% of the current ice loss in Greenland. The glacial history of GIC s is not well constrained, however, and little is known about how they reacted to Holocene climate changes. Specifically, in North Greenland, there is limited knowledge about past GIC fluctuations and whether they survived the Holocene Thermal Maximum ( HTM , ~8 to 5 ka). In this study, we use proglacial lake records to constrain the ice‐marginal fluctuations of three local ice caps in North Greenland including Flade Isblink, the largest ice cap in Greenland. Additionally, we have radiocarbon dated reworked marine molluscs in Little Ice Age ( LIA ) moraines adjacent to the Flade Isblink, which reveal when the ice cap was smaller than present. We found that outlet glaciers from Flade Isblink retreated inland of their present extent from ~9.4 to 0.2 cal. ka BP . The proglacial lake records, however, demonstrate that the lakes continued to receive glacial meltwater throughout the entire Holocene. This implies that GIC s in Finderup Land survived the HTM . Our results are consistent with other observations from North Greenland but differ from locations in southern Greenland where all records show that the local ice caps at low and intermediate elevations disappeared completely during the HTM . We explain the north–south gradient in glacier response as a result of sensitivity to increased temperature and precipitation. While the increased temperatures during the HTM led to a complete melting of GIC s in southern Greenland, GIC s remained in North Greenland probably because the melting was counterbalanced by increased precipitation due to a reduction in Arctic sea‐ice extent and/or increased poleward moisture transport. Article in Journal/Newspaper Arctic glacier Greenland Ice cap North Greenland Sea ice Wiley Online Library Arctic Flade Isblink ENVELOPE(-15.000,-15.000,81.583,81.583) Greenland Boreas 48 3 551 562 |
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Open Polar |
collection |
Wiley Online Library |
op_collection_id |
crwiley |
language |
English |
description |
Local glaciers and ice caps ( GIC s) comprise only ~5.4% of the total ice volume, but account for ~14–20% of the current ice loss in Greenland. The glacial history of GIC s is not well constrained, however, and little is known about how they reacted to Holocene climate changes. Specifically, in North Greenland, there is limited knowledge about past GIC fluctuations and whether they survived the Holocene Thermal Maximum ( HTM , ~8 to 5 ka). In this study, we use proglacial lake records to constrain the ice‐marginal fluctuations of three local ice caps in North Greenland including Flade Isblink, the largest ice cap in Greenland. Additionally, we have radiocarbon dated reworked marine molluscs in Little Ice Age ( LIA ) moraines adjacent to the Flade Isblink, which reveal when the ice cap was smaller than present. We found that outlet glaciers from Flade Isblink retreated inland of their present extent from ~9.4 to 0.2 cal. ka BP . The proglacial lake records, however, demonstrate that the lakes continued to receive glacial meltwater throughout the entire Holocene. This implies that GIC s in Finderup Land survived the HTM . Our results are consistent with other observations from North Greenland but differ from locations in southern Greenland where all records show that the local ice caps at low and intermediate elevations disappeared completely during the HTM . We explain the north–south gradient in glacier response as a result of sensitivity to increased temperature and precipitation. While the increased temperatures during the HTM led to a complete melting of GIC s in southern Greenland, GIC s remained in North Greenland probably because the melting was counterbalanced by increased precipitation due to a reduction in Arctic sea‐ice extent and/or increased poleward moisture transport. |
author2 |
Arctic Research Centre Aarhus University Villum Young Investigator Programme |
format |
Article in Journal/Newspaper |
author |
Larsen, Nicolaj K. Levy, Laura B. Strunk, Astrid Søndergaard, Anne Sofie Olsen, Jesper Lauridsen, Torben L. |
spellingShingle |
Larsen, Nicolaj K. Levy, Laura B. Strunk, Astrid Søndergaard, Anne Sofie Olsen, Jesper Lauridsen, Torben L. Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
author_facet |
Larsen, Nicolaj K. Levy, Laura B. Strunk, Astrid Søndergaard, Anne Sofie Olsen, Jesper Lauridsen, Torben L. |
author_sort |
Larsen, Nicolaj K. |
title |
Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
title_short |
Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
title_full |
Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
title_fullStr |
Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
title_full_unstemmed |
Local ice caps in Finderup Land, North Greenland, survived the Holocene Thermal Maximum |
title_sort |
local ice caps in finderup land, north greenland, survived the holocene thermal maximum |
publisher |
Wiley |
publishDate |
2019 |
url |
http://dx.doi.org/10.1111/bor.12384 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fbor.12384 https://onlinelibrary.wiley.com/doi/pdf/10.1111/bor.12384 https://onlinelibrary.wiley.com/doi/full-xml/10.1111/bor.12384 |
long_lat |
ENVELOPE(-15.000,-15.000,81.583,81.583) |
geographic |
Arctic Flade Isblink Greenland |
geographic_facet |
Arctic Flade Isblink Greenland |
genre |
Arctic glacier Greenland Ice cap North Greenland Sea ice |
genre_facet |
Arctic glacier Greenland Ice cap North Greenland Sea ice |
op_source |
Boreas volume 48, issue 3, page 551-562 ISSN 0300-9483 1502-3885 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/bor.12384 |
container_title |
Boreas |
container_volume |
48 |
container_issue |
3 |
container_start_page |
551 |
op_container_end_page |
562 |
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1800747122673319936 |