Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ...
<!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated...
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ftdatacite:10.57757/iugg23-2465 2023-07-23T04:21:53+02:00 Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... Yang, Ji-Woong Ladant, Jean-Baptiste Landais, Amaëlle Blunier, Thomas Kageyama, Masa Jaccard, Samuel Duchamp-Alphonse, Stéphanie Sánchez Goñi, María Fernanda Prié, Frédéric 2023 https://dx.doi.org/10.57757/iugg23-2465 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018287 unknown GFZ German Research Centre for Geosciences Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Article ConferencePaper Oral 2023 ftdatacite https://doi.org/10.57757/iugg23-2465 2023-07-03T17:36:25Z <!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated millennial-scale atmospheric CO 2 variations characterized by rapid shifts between relatively cold (stadial) and warm (interstadial) stages and in particular, a gradual rising of CO 2 during Heinrich Stadials (HS). To date, the observed CO 2 increase during HS has been attributed to ventilation changes in Southern Ocean, and/or reduced biological uptake. However, understanding the respective contribution of ocean ventilation and changes in the efficiency of the biological carbon pump is challenging because of difficulties in estimating global biosphere productivity based on local reconstructions as they are often based on indirect geochemical tracers and exhibit spatial heterogeneities. To address this, we ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... Conference Object Southern Ocean DataCite Metadata Store (German National Library of Science and Technology) Southern Ocean |
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Open Polar |
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DataCite Metadata Store (German National Library of Science and Technology) |
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description |
<!--!introduction!--> The last glacial period was punctuated by a number of transient events during which massive iceberg discharges profoundly perturbed the deep ocean circulation dynamics, causing widespread climate and environmental changes. Detailed analysis of polar ice cores demonstrated millennial-scale atmospheric CO 2 variations characterized by rapid shifts between relatively cold (stadial) and warm (interstadial) stages and in particular, a gradual rising of CO 2 during Heinrich Stadials (HS). To date, the observed CO 2 increase during HS has been attributed to ventilation changes in Southern Ocean, and/or reduced biological uptake. However, understanding the respective contribution of ocean ventilation and changes in the efficiency of the biological carbon pump is challenging because of difficulties in estimating global biosphere productivity based on local reconstructions as they are often based on indirect geochemical tracers and exhibit spatial heterogeneities. To address this, we ... : The 28th IUGG General Assembly (IUGG2023) (Berlin 2023) ... |
format |
Conference Object |
author |
Yang, Ji-Woong Ladant, Jean-Baptiste Landais, Amaëlle Blunier, Thomas Kageyama, Masa Jaccard, Samuel Duchamp-Alphonse, Stéphanie Sánchez Goñi, María Fernanda Prié, Frédéric |
spellingShingle |
Yang, Ji-Woong Ladant, Jean-Baptiste Landais, Amaëlle Blunier, Thomas Kageyama, Masa Jaccard, Samuel Duchamp-Alphonse, Stéphanie Sánchez Goñi, María Fernanda Prié, Frédéric Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
author_facet |
Yang, Ji-Woong Ladant, Jean-Baptiste Landais, Amaëlle Blunier, Thomas Kageyama, Masa Jaccard, Samuel Duchamp-Alphonse, Stéphanie Sánchez Goñi, María Fernanda Prié, Frédéric |
author_sort |
Yang, Ji-Woong |
title |
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
title_short |
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
title_full |
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
title_fullStr |
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
title_full_unstemmed |
Global biosphere productivity changes during Heinrich Stadial 4: Preliminary results from the triple O2 isotopes and coupled climate model simulations ... |
title_sort |
global biosphere productivity changes during heinrich stadial 4: preliminary results from the triple o2 isotopes and coupled climate model simulations ... |
publisher |
GFZ German Research Centre for Geosciences |
publishDate |
2023 |
url |
https://dx.doi.org/10.57757/iugg23-2465 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018287 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.57757/iugg23-2465 |
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1772188216719310848 |