Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements

Nitrogen and argon stable isotope data obtained from ancient air in ice cores provide the opportunity to reconstruct past temperatures in Greenland. In this study, we use a recently developed fitting-algorithm based on a Monte Carlo inversion technique coupled with two firn densification and heat di...

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Published in:Quaternary Science Reviews
Main Authors: Döring, Michael, Leuenberger, Markus
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2022
Subjects:
Online Access:https://boris.unibe.ch/194862/1/1-s2.0-S0277379121004819-main.pdf
https://boris.unibe.ch/194862/
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spelling ftunivbern:oai:boris.unibe.ch:194862 2024-04-28T08:21:51+00:00 Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements Döring, Michael Leuenberger, Markus 2022-03-15 application/pdf https://boris.unibe.ch/194862/1/1-s2.0-S0277379121004819-main.pdf https://boris.unibe.ch/194862/ eng eng Elsevier https://boris.unibe.ch/194862/ info:eu-repo/semantics/openAccess Döring, Michael; Leuenberger, Markus (2022). Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements. Quaternary science reviews, 280 Elsevier 10.1016/j.quascirev.2021.107274 <http://dx.doi.org/10.1016/j.quascirev.2021.107274> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2022 ftunivbern https://doi.org/10.1016/j.quascirev.2021.107274 2024-04-03T14:10:36Z Nitrogen and argon stable isotope data obtained from ancient air in ice cores provide the opportunity to reconstruct past temperatures in Greenland. In this study, we use a recently developed fitting-algorithm based on a Monte Carlo inversion technique coupled with two firn densification and heat diffusion models to fit several Holocene gas-isotope data measured at the GISP2 ice core and infer temperature variations. We present for the first time the resulting temperature estimates when fitting δ15N, δ40Ar, and δ15Nexcess as individual targets. While the comparison between the reconstructions using δ15N and δ40Ar shows high agreement, the use of δ15Nexcess for temperature reconstruction is problematic because the statistical and systematic data uncertainty is higher and has a particular impact on multi-decadal to multi-centennial signals. Our analyses demonstrate that T(δ15N) provides the most robust estimate. The T(δ15N) estimate is in better agreement with Buizert et al. (2018) than with the temperature reconstruction of Kobashi et al. (2017). However, all three reconstruction strategies lead to different temperature realizations. Article in Journal/Newspaper Greenland ice core BORIS (Bern Open Repository and Information System, University of Bern) Quaternary Science Reviews 280 107274
institution Open Polar
collection BORIS (Bern Open Repository and Information System, University of Bern)
op_collection_id ftunivbern
language English
topic 530 Physics
spellingShingle 530 Physics
Döring, Michael
Leuenberger, Markus
Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
topic_facet 530 Physics
description Nitrogen and argon stable isotope data obtained from ancient air in ice cores provide the opportunity to reconstruct past temperatures in Greenland. In this study, we use a recently developed fitting-algorithm based on a Monte Carlo inversion technique coupled with two firn densification and heat diffusion models to fit several Holocene gas-isotope data measured at the GISP2 ice core and infer temperature variations. We present for the first time the resulting temperature estimates when fitting δ15N, δ40Ar, and δ15Nexcess as individual targets. While the comparison between the reconstructions using δ15N and δ40Ar shows high agreement, the use of δ15Nexcess for temperature reconstruction is problematic because the statistical and systematic data uncertainty is higher and has a particular impact on multi-decadal to multi-centennial signals. Our analyses demonstrate that T(δ15N) provides the most robust estimate. The T(δ15N) estimate is in better agreement with Buizert et al. (2018) than with the temperature reconstruction of Kobashi et al. (2017). However, all three reconstruction strategies lead to different temperature realizations.
format Article in Journal/Newspaper
author Döring, Michael
Leuenberger, Markus
author_facet Döring, Michael
Leuenberger, Markus
author_sort Döring, Michael
title Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
title_short Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
title_full Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
title_fullStr Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
title_full_unstemmed Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements
title_sort comparison of holocene temperature reconstructions based on gisp2 multiple-gas-isotope measurements
publisher Elsevier
publishDate 2022
url https://boris.unibe.ch/194862/1/1-s2.0-S0277379121004819-main.pdf
https://boris.unibe.ch/194862/
genre Greenland
ice core
genre_facet Greenland
ice core
op_source Döring, Michael; Leuenberger, Markus (2022). Comparison of Holocene temperature reconstructions based on GISP2 multiple-gas-isotope measurements. Quaternary science reviews, 280 Elsevier 10.1016/j.quascirev.2021.107274 <http://dx.doi.org/10.1016/j.quascirev.2021.107274>
op_relation https://boris.unibe.ch/194862/
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1016/j.quascirev.2021.107274
container_title Quaternary Science Reviews
container_volume 280
container_start_page 107274
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