Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations
Anthropogenic CO 2 emissions cause irreversible climate change on centennial to millennial timescales, yet current mitigation efforts are insufficient to limit global warming to a level that is considered safe. Carbon dioxide removal (CDR) has been suggested as an option to partially reverse climate...
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ftcopernicus:oai:publications.copernicus.org:esd105512 2023-05-15T17:57:20+02:00 Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations Schwinger, Jörg Asaadi, Ali Steinert, Norman Julius Lee, Hanna 2022-11-23 application/pdf https://doi.org/10.5194/esd-13-1641-2022 https://esd.copernicus.org/articles/13/1641/2022/ eng eng doi:10.5194/esd-13-1641-2022 https://esd.copernicus.org/articles/13/1641/2022/ eISSN: 2190-4987 Text 2022 ftcopernicus https://doi.org/10.5194/esd-13-1641-2022 2022-11-28T17:22:42Z Anthropogenic CO 2 emissions cause irreversible climate change on centennial to millennial timescales, yet current mitigation efforts are insufficient to limit global warming to a level that is considered safe. Carbon dioxide removal (CDR) has been suggested as an option to partially reverse climate change and to return the Earth system to a less dangerous state after a period of temperature overshoot. Whether or to what extent such partial reversal of climate change under CDR would happen is, next to socio-economic feasibility and sustainability, key to assessing CDR as a mitigation option. Here, we use a state-of-the-art Earth system model that includes a representation of permafrost carbon to investigate the reversibility of the Earth system after overshoots of different durations and magnitudes in idealized simulations. We find that atmospheric CO 2 concentrations are slightly lower after an overshoot, compared to a reference simulation without overshoot, due to a near-perfect compensation of carbon losses from land by increased ocean carbon uptake during the overshoot periods. The legacy of an overshoot is, on a centennial timescale, indiscernible (within natural variability) from a reference case without overshoot for many aspects of the Earth system including global average surface temperature, marine and terrestrial productivity, strength of the Atlantic meridional overturning circulation, surface ocean pH, surface O 2 concentration, and permafrost extent, except in the most extreme overshoot scenario considered in this study. Consistent with previous studies, we find irreversibility in permafrost carbon and deep ocean properties like seawater temperature, pH, and O 2 concentrations. We do not find any indication of tipping points or self-reinforcing feedbacks that would put the Earth system on a significantly different trajectory after an overshoot. Hence, the effectiveness of CDR in partially reversing large-scale patterns of climate change might not be the main issue of CDR but rather the impacts and ... Text permafrost Copernicus Publications: E-Journals Earth System Dynamics 13 4 1641 1665 |
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English |
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Anthropogenic CO 2 emissions cause irreversible climate change on centennial to millennial timescales, yet current mitigation efforts are insufficient to limit global warming to a level that is considered safe. Carbon dioxide removal (CDR) has been suggested as an option to partially reverse climate change and to return the Earth system to a less dangerous state after a period of temperature overshoot. Whether or to what extent such partial reversal of climate change under CDR would happen is, next to socio-economic feasibility and sustainability, key to assessing CDR as a mitigation option. Here, we use a state-of-the-art Earth system model that includes a representation of permafrost carbon to investigate the reversibility of the Earth system after overshoots of different durations and magnitudes in idealized simulations. We find that atmospheric CO 2 concentrations are slightly lower after an overshoot, compared to a reference simulation without overshoot, due to a near-perfect compensation of carbon losses from land by increased ocean carbon uptake during the overshoot periods. The legacy of an overshoot is, on a centennial timescale, indiscernible (within natural variability) from a reference case without overshoot for many aspects of the Earth system including global average surface temperature, marine and terrestrial productivity, strength of the Atlantic meridional overturning circulation, surface ocean pH, surface O 2 concentration, and permafrost extent, except in the most extreme overshoot scenario considered in this study. Consistent with previous studies, we find irreversibility in permafrost carbon and deep ocean properties like seawater temperature, pH, and O 2 concentrations. We do not find any indication of tipping points or self-reinforcing feedbacks that would put the Earth system on a significantly different trajectory after an overshoot. Hence, the effectiveness of CDR in partially reversing large-scale patterns of climate change might not be the main issue of CDR but rather the impacts and ... |
format |
Text |
author |
Schwinger, Jörg Asaadi, Ali Steinert, Norman Julius Lee, Hanna |
spellingShingle |
Schwinger, Jörg Asaadi, Ali Steinert, Norman Julius Lee, Hanna Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
author_facet |
Schwinger, Jörg Asaadi, Ali Steinert, Norman Julius Lee, Hanna |
author_sort |
Schwinger, Jörg |
title |
Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
title_short |
Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
title_full |
Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
title_fullStr |
Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
title_full_unstemmed |
Emit now, mitigate later? Earth system reversibility under overshoots of different magnitudes and durations |
title_sort |
emit now, mitigate later? earth system reversibility under overshoots of different magnitudes and durations |
publishDate |
2022 |
url |
https://doi.org/10.5194/esd-13-1641-2022 https://esd.copernicus.org/articles/13/1641/2022/ |
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permafrost |
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permafrost |
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eISSN: 2190-4987 |
op_relation |
doi:10.5194/esd-13-1641-2022 https://esd.copernicus.org/articles/13/1641/2022/ |
op_doi |
https://doi.org/10.5194/esd-13-1641-2022 |
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Earth System Dynamics |
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13 |
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4 |
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1641 |
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1665 |
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