The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature

Abstract The ocean's immense ability to store and release heat on centennial to millennial time scales modulates the impacts of climate perturbations. To gain a better understanding of past variations in mean ocean temperature (MOT), a noble gas‐based proxy measured from ancient air in ice core...

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Published in:Geophysical Research Letters
Main Authors: Frerk Pöppelmeier, Daniel Baggenstos, Markus Grimmer, Zhijun Liu, Jochen Schmitt, Hubertus Fischer, Thomas F. Stocker
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://doi.org/10.1029/2022GL102055
https://doaj.org/article/0a335140f3ea4930bcbc6de3606c1ba2
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spelling ftdoajarticles:oai:doaj.org/article:0a335140f3ea4930bcbc6de3606c1ba2 2024-09-09T19:44:54+00:00 The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature Frerk Pöppelmeier Daniel Baggenstos Markus Grimmer Zhijun Liu Jochen Schmitt Hubertus Fischer Thomas F. Stocker 2023-03-01T00:00:00Z https://doi.org/10.1029/2022GL102055 https://doaj.org/article/0a335140f3ea4930bcbc6de3606c1ba2 EN eng Wiley https://doi.org/10.1029/2022GL102055 https://doaj.org/toc/0094-8276 https://doaj.org/toc/1944-8007 1944-8007 0094-8276 doi:10.1029/2022GL102055 https://doaj.org/article/0a335140f3ea4930bcbc6de3606c1ba2 Geophysical Research Letters, Vol 50, Iss 6, Pp n/a-n/a (2023) mean ocean temperature last glacial maximum noble gases ocean modeling Geophysics. Cosmic physics QC801-809 article 2023 ftdoajarticles https://doi.org/10.1029/2022GL102055 2024-08-05T17:49:23Z Abstract The ocean's immense ability to store and release heat on centennial to millennial time scales modulates the impacts of climate perturbations. To gain a better understanding of past variations in mean ocean temperature (MOT), a noble gas‐based proxy measured from ancient air in ice cores has been developed. Here we assess non‐temperature effects that may influence the atmospheric noble gas ratios reconstructed from polar ice and how they impact the temperature signal with an intermediate complexity Earth system model. We find that changes in wind speed, sea‐ice extent, and ocean circulation have partially compensating effects on mean‐ocean noble gas saturation, leading to a slight reduction of noble gas undersaturation at the Last Glacial Maximum (LGM). Taking these effects and ice core measurements into account, our model suggests a revised MOT difference between the LGM and pre‐industrial of −2.1 ± 0.7°C that is also in improved agreement with other independent temperature reconstructions. Article in Journal/Newspaper ice core Sea ice Directory of Open Access Journals: DOAJ Articles Geophysical Research Letters 50 6
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic mean ocean temperature
last glacial maximum
noble gases
ocean modeling
Geophysics. Cosmic physics
QC801-809
spellingShingle mean ocean temperature
last glacial maximum
noble gases
ocean modeling
Geophysics. Cosmic physics
QC801-809
Frerk Pöppelmeier
Daniel Baggenstos
Markus Grimmer
Zhijun Liu
Jochen Schmitt
Hubertus Fischer
Thomas F. Stocker
The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
topic_facet mean ocean temperature
last glacial maximum
noble gases
ocean modeling
Geophysics. Cosmic physics
QC801-809
description Abstract The ocean's immense ability to store and release heat on centennial to millennial time scales modulates the impacts of climate perturbations. To gain a better understanding of past variations in mean ocean temperature (MOT), a noble gas‐based proxy measured from ancient air in ice cores has been developed. Here we assess non‐temperature effects that may influence the atmospheric noble gas ratios reconstructed from polar ice and how they impact the temperature signal with an intermediate complexity Earth system model. We find that changes in wind speed, sea‐ice extent, and ocean circulation have partially compensating effects on mean‐ocean noble gas saturation, leading to a slight reduction of noble gas undersaturation at the Last Glacial Maximum (LGM). Taking these effects and ice core measurements into account, our model suggests a revised MOT difference between the LGM and pre‐industrial of −2.1 ± 0.7°C that is also in improved agreement with other independent temperature reconstructions.
format Article in Journal/Newspaper
author Frerk Pöppelmeier
Daniel Baggenstos
Markus Grimmer
Zhijun Liu
Jochen Schmitt
Hubertus Fischer
Thomas F. Stocker
author_facet Frerk Pöppelmeier
Daniel Baggenstos
Markus Grimmer
Zhijun Liu
Jochen Schmitt
Hubertus Fischer
Thomas F. Stocker
author_sort Frerk Pöppelmeier
title The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
title_short The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
title_full The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
title_fullStr The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
title_full_unstemmed The Effect of Past Saturation Changes on Noble Gas Reconstructions of Mean Ocean Temperature
title_sort effect of past saturation changes on noble gas reconstructions of mean ocean temperature
publisher Wiley
publishDate 2023
url https://doi.org/10.1029/2022GL102055
https://doaj.org/article/0a335140f3ea4930bcbc6de3606c1ba2
genre ice core
Sea ice
genre_facet ice core
Sea ice
op_source Geophysical Research Letters, Vol 50, Iss 6, Pp n/a-n/a (2023)
op_relation https://doi.org/10.1029/2022GL102055
https://doaj.org/toc/0094-8276
https://doaj.org/toc/1944-8007
1944-8007
0094-8276
doi:10.1029/2022GL102055
https://doaj.org/article/0a335140f3ea4930bcbc6de3606c1ba2
op_doi https://doi.org/10.1029/2022GL102055
container_title Geophysical Research Letters
container_volume 50
container_issue 6
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