Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core
In order to reconstruct the temperature of the North Greenland Ice Core Project (NGRIP) site, new measurements of δ 15 N have been performed covering the time period from the beginning of the Holocene to Dansgaard–Oeschger (DO) event 8. Together with previously measured and mostly published δ 15 N d...
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ftcopernicus:oai:publications.copernicus.org:cp21091 2023-05-15T16:29:37+02:00 Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core Kindler, P. Guillevic, M. Baumgartner, M. Schwander, J. Landais, A. Leuenberger, M. 2018-09-27 application/pdf https://doi.org/10.5194/cp-10-887-2014 https://cp.copernicus.org/articles/10/887/2014/ eng eng doi:10.5194/cp-10-887-2014 https://cp.copernicus.org/articles/10/887/2014/ eISSN: 1814-9332 Text 2018 ftcopernicus https://doi.org/10.5194/cp-10-887-2014 2020-07-20T16:25:07Z In order to reconstruct the temperature of the North Greenland Ice Core Project (NGRIP) site, new measurements of δ 15 N have been performed covering the time period from the beginning of the Holocene to Dansgaard–Oeschger (DO) event 8. Together with previously measured and mostly published δ 15 N data, we present for the first time a NGRIP temperature reconstruction for the whole last glacial period from 10 to 120 kyr b2k (thousand years before 2000 AD) including every DO event based on δ 15 N isotope measurements combined with a firn densification and heat diffusion model. The detected temperature rises at the onset of DO events range from 5 °C (DO 25) up to 16.5 °C (DO 11) with an uncertainty of ±3 °C. To bring measured and modelled data into agreement, we had to reduce the accumulation rate given by the NGRIP ss09sea06bm timescale in some periods by 30 to 35%, especially during the last glacial maximum. A comparison between reconstructed temperature and δ 18 O ice data confirms that the isotopic composition of the stadial was strongly influenced by seasonality. We evidence an anticorrelation between the variations of the δ 18 O ice sensitivity to temperature (referred to as α) and obliquity in agreement with a simple Rayleigh distillation model. Finally, we suggest that α might be influenced by the Northern Hemisphere ice sheet volume. Text Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project Copernicus Publications: E-Journals Greenland Climate of the Past 10 2 887 902 |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
In order to reconstruct the temperature of the North Greenland Ice Core Project (NGRIP) site, new measurements of δ 15 N have been performed covering the time period from the beginning of the Holocene to Dansgaard–Oeschger (DO) event 8. Together with previously measured and mostly published δ 15 N data, we present for the first time a NGRIP temperature reconstruction for the whole last glacial period from 10 to 120 kyr b2k (thousand years before 2000 AD) including every DO event based on δ 15 N isotope measurements combined with a firn densification and heat diffusion model. The detected temperature rises at the onset of DO events range from 5 °C (DO 25) up to 16.5 °C (DO 11) with an uncertainty of ±3 °C. To bring measured and modelled data into agreement, we had to reduce the accumulation rate given by the NGRIP ss09sea06bm timescale in some periods by 30 to 35%, especially during the last glacial maximum. A comparison between reconstructed temperature and δ 18 O ice data confirms that the isotopic composition of the stadial was strongly influenced by seasonality. We evidence an anticorrelation between the variations of the δ 18 O ice sensitivity to temperature (referred to as α) and obliquity in agreement with a simple Rayleigh distillation model. Finally, we suggest that α might be influenced by the Northern Hemisphere ice sheet volume. |
format |
Text |
author |
Kindler, P. Guillevic, M. Baumgartner, M. Schwander, J. Landais, A. Leuenberger, M. |
spellingShingle |
Kindler, P. Guillevic, M. Baumgartner, M. Schwander, J. Landais, A. Leuenberger, M. Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
author_facet |
Kindler, P. Guillevic, M. Baumgartner, M. Schwander, J. Landais, A. Leuenberger, M. |
author_sort |
Kindler, P. |
title |
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
title_short |
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
title_full |
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
title_fullStr |
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
title_full_unstemmed |
Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core |
title_sort |
temperature reconstruction from 10 to 120 kyr b2k from the ngrip ice core |
publishDate |
2018 |
url |
https://doi.org/10.5194/cp-10-887-2014 https://cp.copernicus.org/articles/10/887/2014/ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project |
genre_facet |
Greenland Greenland ice core Greenland Ice core Project ice core Ice Sheet NGRIP North Greenland North Greenland Ice Core Project |
op_source |
eISSN: 1814-9332 |
op_relation |
doi:10.5194/cp-10-887-2014 https://cp.copernicus.org/articles/10/887/2014/ |
op_doi |
https://doi.org/10.5194/cp-10-887-2014 |
container_title |
Climate of the Past |
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10 |
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2 |
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887 |
op_container_end_page |
902 |
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1766019329059454976 |