Articles | Volume 9, issue 2
https://doi.org/10.5194/esd-9-797-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/esd-9-797-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
13 Jun 2018
Research article | Highlight paper |
| 13 Jun 2018
| 13 Jun 2018
Hazards of decreasing marine oxygen: the near-term and millennial-scale benefits of meeting the Paris climate targets
Gianna Battaglia
CORRESPONDING AUTHOR
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
Fortunat Joos
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland
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Cited
22 citations as recorded by crossref.
- Ocean phosphorus inventory: large uncertainties in future projections on millennial timescales and their consequences for ocean deoxygenation T. Kemena et al. 10.5194/esd-10-539-2019
- Is deoxygenation detectable before warming in the thermocline? A. Hameau et al. 10.5194/bg-17-1877-2020
- A committed fourfold increase in ocean oxygen loss A. Oschlies 10.1038/s41467-021-22584-4
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Scenarios of Deoxygenation of the Eastern Tropical North Pacific During the Past Millennium as a Window Into the Future of Oxygen Minimum Zones K. Choumiline et al. 10.3389/feart.2019.00237
- Contrasting Upper and Deep Ocean Oxygen Response to Protracted Global Warming T. Frölicher et al. 10.1029/2020GB006601
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- Climate change-related warming reduces thermal sensitivity and modifies metabolic activity of coastal benthic bacterial communities L. Seidel et al. 10.1038/s41396-023-01395-z
- Hysteresis of the Earth system under positive and negative CO2 emissions A. Jeltsch-Thömmes et al. 10.1088/1748-9326/abc4af
- 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
- The quiet crossing of ocean tipping points C. Heinze et al. 10.1073/pnas.2008478118
- Earth system responses to carbon dioxide removal as exemplified by ocean alkalinity enhancement: tradeoffs and lags A. Jeltsch-Thömmes et al. 10.1088/1748-9326/ad4401
- Assessment of time of emergence of anthropogenic deoxygenation and warming: insights from a CESM simulation from 850 to 2100 CE A. Hameau et al. 10.5194/bg-16-1755-2019
- 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
- The commonly overlooked environmental tipping points G. McPherson et al. 10.1016/j.rineng.2023.101118
- Decadal vision in oceanography 2021: Tropical oceans T. Doi et al. 10.5928/kaiyou.30.5_105
- Geochemical proxies for deep-sea temperature and nutrient content in cold-water bamboo corals T. Williams et al. 10.1016/j.chemgeo.2024.122053
- Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations G. Battaglia & F. Joos 10.1002/2017GB005671
- Global Warming Can Lead to Depletion of Oxygen by Disrupting Phytoplankton Photosynthesis: A Mathematical Modelling Approach Y. Sekerci & S. Petrovskii 10.3390/geosciences8060201
- Pattern Formation in a Model Oxygen-Plankton System Y. Sekerci & S. Petrovskii 10.3390/computation6040059
- Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances A. Jeltsch-Thömmes & F. Joos 10.5194/cp-16-423-2020
- A two-timescale model of plankton–oxygen dynamics predicts formation of oxygen minimum zones and global anoxia P. Roy Chowdhury et al. 10.1007/s00285-024-02107-7
17 citations as recorded by crossref.
- Ocean phosphorus inventory: large uncertainties in future projections on millennial timescales and their consequences for ocean deoxygenation T. Kemena et al. 10.5194/esd-10-539-2019
- Is deoxygenation detectable before warming in the thermocline? A. Hameau et al. 10.5194/bg-17-1877-2020
- A committed fourfold increase in ocean oxygen loss A. Oschlies 10.1038/s41467-021-22584-4
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Scenarios of Deoxygenation of the Eastern Tropical North Pacific During the Past Millennium as a Window Into the Future of Oxygen Minimum Zones K. Choumiline et al. 10.3389/feart.2019.00237
- Contrasting Upper and Deep Ocean Oxygen Response to Protracted Global Warming T. Frölicher et al. 10.1029/2020GB006601
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- Climate change-related warming reduces thermal sensitivity and modifies metabolic activity of coastal benthic bacterial communities L. Seidel et al. 10.1038/s41396-023-01395-z
- Hysteresis of the Earth system under positive and negative CO2 emissions A. Jeltsch-Thömmes et al. 10.1088/1748-9326/abc4af
- 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
- The quiet crossing of ocean tipping points C. Heinze et al. 10.1073/pnas.2008478118
- Earth system responses to carbon dioxide removal as exemplified by ocean alkalinity enhancement: tradeoffs and lags A. Jeltsch-Thömmes et al. 10.1088/1748-9326/ad4401
- Assessment of time of emergence of anthropogenic deoxygenation and warming: insights from a CESM simulation from 850 to 2100 CE A. Hameau et al. 10.5194/bg-16-1755-2019
- 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
- The commonly overlooked environmental tipping points G. McPherson et al. 10.1016/j.rineng.2023.101118
- Decadal vision in oceanography 2021: Tropical oceans T. Doi et al. 10.5928/kaiyou.30.5_105
- Geochemical proxies for deep-sea temperature and nutrient content in cold-water bamboo corals T. Williams et al. 10.1016/j.chemgeo.2024.122053
5 citations as recorded by crossref.
- Marine N2O Emissions From Nitrification and Denitrification Constrained by Modern Observations and Projected in Multimillennial Global Warming Simulations G. Battaglia & F. Joos 10.1002/2017GB005671
- Global Warming Can Lead to Depletion of Oxygen by Disrupting Phytoplankton Photosynthesis: A Mathematical Modelling Approach Y. Sekerci & S. Petrovskii 10.3390/geosciences8060201
- Pattern Formation in a Model Oxygen-Plankton System Y. Sekerci & S. Petrovskii 10.3390/computation6040059
- Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances A. Jeltsch-Thömmes & F. Joos 10.5194/cp-16-423-2020
- A two-timescale model of plankton–oxygen dynamics predicts formation of oxygen minimum zones and global anoxia P. Roy Chowdhury et al. 10.1007/s00285-024-02107-7
Latest update: 20 Nov 2024
Short summary
Human-caused, climate change hazards in the ocean continue to aggravate over a very long time. For business as usual, we project the ocean oxygen content to decrease by 40 % over the next thousand years. This would likely have severe consequences for marine life. Global warming and oxygen loss are linked, and meeting the warming target of the Paris Climate Agreement effectively limits related marine hazards. Developments over many thousands of years should be considered to assess marine risks.
Human-caused, climate change hazards in the ocean continue to aggravate over a very long time....
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