Articles | Volume 17, issue 13
https://doi.org/10.5194/bg-17-3511-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-17-3511-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
N2O changes from the Last Glacial Maximum to the preindustrial – Part 2: terrestrial N2O emissions and carbon–nitrogen cycle interactions
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
Renato Spahni
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
Benjamin D. Stocker
Department of Environmental Systems Science, ETH, Universitätsstrasse 2, 8092 Zurich, Switzerland
Swiss Federal Institute for Forest, Snow and Landscape Research WSL, Zürcherstrasse 111, 8903 Birmensdorf, Switzerland
Sebastian Lienert
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
Jurek Müller
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
Hubertus Fischer
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
Jochen Schmitt
Climate and Environmental Physics, Physics Institute and Oeschger
Centre for Climate Change Research, University of Bern, Bern, 3012,
Switzerland
I. Colin Prentice
AXA Chair of Biosphere and Climate Impacts, Department of Life
Sciences, Imperial College London, Silwood Park Campus, Buckhurst Road, Ascot
SL5 7PY, UK
Ministry of Education Key Laboratory for Earth System Modelling,
Department of Earth System Science, Tsinghua University, Beijing 100084,
China
Department of Biological Sciences, Macquarie University, NSW 2109,
Australia
Bette Otto-Bliesner
Climate and Global Dynamics Laboratory, National Center for Atmospheric
Research, Boulder, CO 80307-3000, USA
Zhengyu Liu
Atmospheric Science Program, Department of Geography, Ohio State
University, OH 43210, USA
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Cited
8 citations as recorded by crossref.
- CH<sub>4</sub> and N<sub>2</sub>O fluctuations during the penultimate deglaciation L. Schmidely et al. 10.5194/cp-17-1627-2021
- Improving nitrogen fertilizer use efficiency and minimizing losses and global warming potential by optimizing applications and using nitrogen synergists in a maize-wheat rotation J. Wang et al. 10.1016/j.agee.2023.108538
- Global Carbon Budget 2022 P. Friedlingstein et al. 10.5194/essd-14-4811-2022
- Sensitivity of the Tropical Dust Cycle to Glacial Abrupt Climate Changes P. Hopcroft et al. 10.1029/2022GL101197
- Evaluating nitrogen cycling in terrestrial biosphere models: a disconnect between the carbon and nitrogen cycles S. Kou-Giesbrecht et al. 10.5194/esd-14-767-2023
- Global nitrous oxide budget (1980–2020) H. Tian et al. 10.5194/essd-16-2543-2024
- N<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N<sub>2</sub>O stable isotopes in ice cores H. Fischer et al. 10.5194/bg-16-3997-2019
- Marine N2O emissions during a Younger Dryas-like event: the role of meridional overturning, tropical thermocline ventilation, and biological productivity F. Joos et al. 10.1088/1748-9326/ab2353
6 citations as recorded by crossref.
- CH<sub>4</sub> and N<sub>2</sub>O fluctuations during the penultimate deglaciation L. Schmidely et al. 10.5194/cp-17-1627-2021
- Improving nitrogen fertilizer use efficiency and minimizing losses and global warming potential by optimizing applications and using nitrogen synergists in a maize-wheat rotation J. Wang et al. 10.1016/j.agee.2023.108538
- Global Carbon Budget 2022 P. Friedlingstein et al. 10.5194/essd-14-4811-2022
- Sensitivity of the Tropical Dust Cycle to Glacial Abrupt Climate Changes P. Hopcroft et al. 10.1029/2022GL101197
- Evaluating nitrogen cycling in terrestrial biosphere models: a disconnect between the carbon and nitrogen cycles S. Kou-Giesbrecht et al. 10.5194/esd-14-767-2023
- Global nitrous oxide budget (1980–2020) H. Tian et al. 10.5194/essd-16-2543-2024
2 citations as recorded by crossref.
- N<sub>2</sub>O changes from the Last Glacial Maximum to the preindustrial – Part 1: Quantitative reconstruction of terrestrial and marine emissions using N<sub>2</sub>O stable isotopes in ice cores H. Fischer et al. 10.5194/bg-16-3997-2019
- Marine N2O emissions during a Younger Dryas-like event: the role of meridional overturning, tropical thermocline ventilation, and biological productivity F. Joos et al. 10.1088/1748-9326/ab2353
Latest update: 12 Nov 2024
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Short summary
Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N) cycling and N2O emissions over the past 21 000 years are compared with reconstructed N2O emissions. Modelled and reconstructed emissions increased strongly during past abrupt warming events. This evidence appears consistent with a dynamic response of biological N fixation to increasing N demand by ecosystems, thereby reducing N limitation of plant productivity and supporting a land sink for atmospheric CO2.
Results of the first globally resolved simulations of terrestrial carbon and nitrogen (N)...
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