Surface accumulation in Northern Central Greenland during the last 300 years
The internal stratigraphy of snow and ice as imaged by ground-penetrating radar may serve as a source of information on past accumulation. This study presents results from two ground-based radar surveys conducted in Greenland in 2007 and 2015, respectively. The first survey was conducted during the...
Published in: | Annals of Glaciology |
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Cambridge University Press
2020
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ftdoajarticles:oai:doaj.org/article:59e8cfda4f79437f9cc5c60fe54edd05 2023-05-15T13:29:34+02:00 Surface accumulation in Northern Central Greenland during the last 300 years Nanna B. Karlsson Sebastian Razik Maria Hörhold Anna Winter Daniel Steinhage Tobias Binder Olaf Eisen 2020-04-01T00:00:00Z https://doi.org/10.1017/aog.2020.30 https://doaj.org/article/59e8cfda4f79437f9cc5c60fe54edd05 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0260305520000300/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2020.30 0260-3055 1727-5644 https://doaj.org/article/59e8cfda4f79437f9cc5c60fe54edd05 Annals of Glaciology, Vol 61, Pp 214-224 (2020) Accumulation Ground-penetrating radar Ice-sheet mass balance Radio-echo sounding Meteorology. Climatology QC851-999 article 2020 ftdoajarticles https://doi.org/10.1017/aog.2020.30 2023-03-12T01:31:55Z The internal stratigraphy of snow and ice as imaged by ground-penetrating radar may serve as a source of information on past accumulation. This study presents results from two ground-based radar surveys conducted in Greenland in 2007 and 2015, respectively. The first survey was conducted during the traverse from the ice-core station NGRIP (North Greenland Ice Core Project) to the ice-core station NEEM (North Greenland Eemian Ice Drilling). The second survey was carried out during the traverse from NEEM to the ice-core station EGRIP (East Greenland Ice Core Project) and then onwards to Summit Station. The total length of the radar profiles is 1427 km. From the radar data, we retrieve the large-scale spatial variation of the accumulation rates in the interior of the ice sheet. The accumulation rates range from 0.11 to 0.26 m a−1 ice equivalent with the lowest values found in the northeastern sector towards EGRIP. We find no evidence of temporal or spatial changes in accumulation rates when comparing the 150-year average accumulation rates with the 321-year average accumulation rates. Comparisons with regional climate models reveal that the models underestimate accumulation rates by up to 35% in northeastern Greenland. Our results serve as a robust baseline to detect present changes in either surface accumulation rates or patterns. Article in Journal/Newspaper Annals of Glaciology East Greenland East Greenland Ice-core Project Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project Directory of Open Access Journals: DOAJ Articles Greenland Annals of Glaciology 61 81 214 224 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Accumulation Ground-penetrating radar Ice-sheet mass balance Radio-echo sounding Meteorology. Climatology QC851-999 |
spellingShingle |
Accumulation Ground-penetrating radar Ice-sheet mass balance Radio-echo sounding Meteorology. Climatology QC851-999 Nanna B. Karlsson Sebastian Razik Maria Hörhold Anna Winter Daniel Steinhage Tobias Binder Olaf Eisen Surface accumulation in Northern Central Greenland during the last 300 years |
topic_facet |
Accumulation Ground-penetrating radar Ice-sheet mass balance Radio-echo sounding Meteorology. Climatology QC851-999 |
description |
The internal stratigraphy of snow and ice as imaged by ground-penetrating radar may serve as a source of information on past accumulation. This study presents results from two ground-based radar surveys conducted in Greenland in 2007 and 2015, respectively. The first survey was conducted during the traverse from the ice-core station NGRIP (North Greenland Ice Core Project) to the ice-core station NEEM (North Greenland Eemian Ice Drilling). The second survey was carried out during the traverse from NEEM to the ice-core station EGRIP (East Greenland Ice Core Project) and then onwards to Summit Station. The total length of the radar profiles is 1427 km. From the radar data, we retrieve the large-scale spatial variation of the accumulation rates in the interior of the ice sheet. The accumulation rates range from 0.11 to 0.26 m a−1 ice equivalent with the lowest values found in the northeastern sector towards EGRIP. We find no evidence of temporal or spatial changes in accumulation rates when comparing the 150-year average accumulation rates with the 321-year average accumulation rates. Comparisons with regional climate models reveal that the models underestimate accumulation rates by up to 35% in northeastern Greenland. Our results serve as a robust baseline to detect present changes in either surface accumulation rates or patterns. |
format |
Article in Journal/Newspaper |
author |
Nanna B. Karlsson Sebastian Razik Maria Hörhold Anna Winter Daniel Steinhage Tobias Binder Olaf Eisen |
author_facet |
Nanna B. Karlsson Sebastian Razik Maria Hörhold Anna Winter Daniel Steinhage Tobias Binder Olaf Eisen |
author_sort |
Nanna B. Karlsson |
title |
Surface accumulation in Northern Central Greenland during the last 300 years |
title_short |
Surface accumulation in Northern Central Greenland during the last 300 years |
title_full |
Surface accumulation in Northern Central Greenland during the last 300 years |
title_fullStr |
Surface accumulation in Northern Central Greenland during the last 300 years |
title_full_unstemmed |
Surface accumulation in Northern Central Greenland during the last 300 years |
title_sort |
surface accumulation in northern central greenland during the last 300 years |
publisher |
Cambridge University Press |
publishDate |
2020 |
url |
https://doi.org/10.1017/aog.2020.30 https://doaj.org/article/59e8cfda4f79437f9cc5c60fe54edd05 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Annals of Glaciology East Greenland East Greenland Ice-core Project Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project |
genre_facet |
Annals of Glaciology East Greenland East Greenland Ice-core Project Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project |
op_source |
Annals of Glaciology, Vol 61, Pp 214-224 (2020) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0260305520000300/type/journal_article https://doaj.org/toc/0260-3055 https://doaj.org/toc/1727-5644 doi:10.1017/aog.2020.30 0260-3055 1727-5644 https://doaj.org/article/59e8cfda4f79437f9cc5c60fe54edd05 |
op_doi |
https://doi.org/10.1017/aog.2020.30 |
container_title |
Annals of Glaciology |
container_volume |
61 |
container_issue |
81 |
container_start_page |
214 |
op_container_end_page |
224 |
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1766001246881185792 |