N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ...
Carbon–nitrogen (C–N) interactions regulate N availability for plant growth and for emissions of nitrous oxide (N2O) and the uptake of carbon dioxide. Future projections of these terrestrial greenhouse gas fluxes are strikingly divergent, leading to major uncertainties in projected global warming. H...
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Online Access: | https://dx.doi.org/10.3929/ethz-b-000429152 http://hdl.handle.net/20.500.11850/429152 |
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ftdatacite:10.3929/ethz-b-000429152 2024-04-28T08:24:19+00:00 N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... Joos, Fortunat Spahni, Renato Stocker, Benjamin Lienert, Sebastian Müller, Jurek Fischer, Hubertus Schmitt, Jochen Prentice, I. Colin Otto-Bliesner, Bette Liu, Zhengyu 2020 application/pdf https://dx.doi.org/10.3929/ethz-b-000429152 http://hdl.handle.net/20.500.11850/429152 en eng ETH Zurich info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 article-journal Text ScholarlyArticle Journal Article 2020 ftdatacite https://doi.org/10.3929/ethz-b-000429152 2024-04-02T12:34:54Z Carbon–nitrogen (C–N) interactions regulate N availability for plant growth and for emissions of nitrous oxide (N2O) and the uptake of carbon dioxide. Future projections of these terrestrial greenhouse gas fluxes are strikingly divergent, leading to major uncertainties in projected global warming. Here we analyse the large increase in terrestrial N2O emissions over the past 21 000 years as reconstructed from ice-core isotopic data and presented in part 1 of this study. Remarkably, the increase occurred in two steps, each realized over decades and within a maximum of 2 centuries, at the onsets of the major deglacial Northern Hemisphere warming events. The data suggest a highly dynamic and responsive global N cycle. The increase may be explained by an increase in the flux of reactive N entering and leaving ecosystems or by an increase in N2O yield per unit N converted. We applied the LPX-Bern dynamic global vegetation model in deglacial simulations forced with Earth system model climate data to investigate N2O ... : Biogeosciences, 17 (13) ... Article in Journal/Newspaper ice core DataCite Metadata Store (German National Library of Science and Technology) |
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DataCite Metadata Store (German National Library of Science and Technology) |
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English |
description |
Carbon–nitrogen (C–N) interactions regulate N availability for plant growth and for emissions of nitrous oxide (N2O) and the uptake of carbon dioxide. Future projections of these terrestrial greenhouse gas fluxes are strikingly divergent, leading to major uncertainties in projected global warming. Here we analyse the large increase in terrestrial N2O emissions over the past 21 000 years as reconstructed from ice-core isotopic data and presented in part 1 of this study. Remarkably, the increase occurred in two steps, each realized over decades and within a maximum of 2 centuries, at the onsets of the major deglacial Northern Hemisphere warming events. The data suggest a highly dynamic and responsive global N cycle. The increase may be explained by an increase in the flux of reactive N entering and leaving ecosystems or by an increase in N2O yield per unit N converted. We applied the LPX-Bern dynamic global vegetation model in deglacial simulations forced with Earth system model climate data to investigate N2O ... : Biogeosciences, 17 (13) ... |
format |
Article in Journal/Newspaper |
author |
Joos, Fortunat Spahni, Renato Stocker, Benjamin Lienert, Sebastian Müller, Jurek Fischer, Hubertus Schmitt, Jochen Prentice, I. Colin Otto-Bliesner, Bette Liu, Zhengyu |
spellingShingle |
Joos, Fortunat Spahni, Renato Stocker, Benjamin Lienert, Sebastian Müller, Jurek Fischer, Hubertus Schmitt, Jochen Prentice, I. Colin Otto-Bliesner, Bette Liu, Zhengyu N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
author_facet |
Joos, Fortunat Spahni, Renato Stocker, Benjamin Lienert, Sebastian Müller, Jurek Fischer, Hubertus Schmitt, Jochen Prentice, I. Colin Otto-Bliesner, Bette Liu, Zhengyu |
author_sort |
Joos, Fortunat |
title |
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
title_short |
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
title_full |
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
title_fullStr |
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
title_full_unstemmed |
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions ... |
title_sort |
n2o changes from the last glacial maximum to the preindustrial – part 2: terrestrial n2o emissions and carbon–nitrogen cycle interactions ... |
publisher |
ETH Zurich |
publishDate |
2020 |
url |
https://dx.doi.org/10.3929/ethz-b-000429152 http://hdl.handle.net/20.500.11850/429152 |
genre |
ice core |
genre_facet |
ice core |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.3929/ethz-b-000429152 |
_version_ |
1797584692593033216 |