Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios
The present study investigates the response of the high-latitude carbon cycle to changes in atmospheric greenhouse gas (GHG) concentrations in idealized climate change scenarios. To this end we use an adapted version of JSBACH – the land surface component of the Max Planck Institute for Meteorology...
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2021
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Online Access: | https://oceanrep.geomar.de/id/eprint/52534/ https://oceanrep.geomar.de/id/eprint/52534/1/tc-15-1097-2021.pdf https://doi.org/10.5194/tc-15-1097-2021 |
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ftoceanrep:oai:oceanrep.geomar.de:52534 2023-05-15T17:58:13+02:00 Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios de Vrese, Philipp Stacke, Tobias Kleinen, Thomas Brovkin, Victor 2021-03-02 text https://oceanrep.geomar.de/id/eprint/52534/ https://oceanrep.geomar.de/id/eprint/52534/1/tc-15-1097-2021.pdf https://doi.org/10.5194/tc-15-1097-2021 en eng Copernicus Publications (EGU) https://oceanrep.geomar.de/id/eprint/52534/1/tc-15-1097-2021.pdf de Vrese, P., Stacke, T., Kleinen, T. and Brovkin, V. (2021) Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios. Open Access The Cryosphere, 15 (2). pp. 1097-1130. DOI 10.5194/tc-15-1097-2021 <https://doi.org/10.5194/tc-15-1097-2021>. doi:10.5194/tc-15-1097-2021 cc_by_4.0 info:eu-repo/semantics/openAccess Article PeerReviewed 2021 ftoceanrep https://doi.org/10.5194/tc-15-1097-2021 2023-04-07T15:55:51Z The present study investigates the response of the high-latitude carbon cycle to changes in atmospheric greenhouse gas (GHG) concentrations in idealized climate change scenarios. To this end we use an adapted version of JSBACH – the land surface component of the Max Planck Institute for Meteorology Earth System Model (MPI-ESM) – that accounts for the organic matter stored in the permafrost-affected soils of the high northern latitudes. The model is run under different climate scenarios that assume an increase in GHG concentrations, based on the Shared Socioeconomic Pathway 5 and the Representative Concentration Pathway 8.5, which peaks in the years 2025, 2050, 2075 or 2100, respectively. The peaks are followed by a decrease in atmospheric GHGs that returns the concentrations to the levels at the beginning of the 21st century, reversing the imposed climate change. We show that the soil CO2 emissions exhibit an almost linear dependence on the global mean surface temperatures that are simulated for the different climate scenarios. Here, each degree of warming increases the fluxes by, very roughly, 50 % of their initial value, while each degree of cooling decreases them correspondingly. However, the linear dependence does not mean that the processes governing the soil CO2 emissions are fully reversible on short timescales but rather that two strongly hysteretic factors offset each other – namely the net primary productivity and the availability of formerly frozen soil organic matter. In contrast, the soil methane emissions show a less pronounced increase with rising temperatures, and they are consistently lower after the peak in the GHG concentrations than prior to it. Here, the net fluxes could even become negative, and we find that methane emissions will play only a minor role in the northern high-latitude contribution to global warming, even when considering the high global warming potential of the gas. Finally, we find that at a global mean temperature of roughly 1.75 K (±0.5 K) above pre-industrial levels the ... Article in Journal/Newspaper permafrost The Cryosphere OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) The Cryosphere 15 2 1097 1130 |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
The present study investigates the response of the high-latitude carbon cycle to changes in atmospheric greenhouse gas (GHG) concentrations in idealized climate change scenarios. To this end we use an adapted version of JSBACH – the land surface component of the Max Planck Institute for Meteorology Earth System Model (MPI-ESM) – that accounts for the organic matter stored in the permafrost-affected soils of the high northern latitudes. The model is run under different climate scenarios that assume an increase in GHG concentrations, based on the Shared Socioeconomic Pathway 5 and the Representative Concentration Pathway 8.5, which peaks in the years 2025, 2050, 2075 or 2100, respectively. The peaks are followed by a decrease in atmospheric GHGs that returns the concentrations to the levels at the beginning of the 21st century, reversing the imposed climate change. We show that the soil CO2 emissions exhibit an almost linear dependence on the global mean surface temperatures that are simulated for the different climate scenarios. Here, each degree of warming increases the fluxes by, very roughly, 50 % of their initial value, while each degree of cooling decreases them correspondingly. However, the linear dependence does not mean that the processes governing the soil CO2 emissions are fully reversible on short timescales but rather that two strongly hysteretic factors offset each other – namely the net primary productivity and the availability of formerly frozen soil organic matter. In contrast, the soil methane emissions show a less pronounced increase with rising temperatures, and they are consistently lower after the peak in the GHG concentrations than prior to it. Here, the net fluxes could even become negative, and we find that methane emissions will play only a minor role in the northern high-latitude contribution to global warming, even when considering the high global warming potential of the gas. Finally, we find that at a global mean temperature of roughly 1.75 K (±0.5 K) above pre-industrial levels the ... |
format |
Article in Journal/Newspaper |
author |
de Vrese, Philipp Stacke, Tobias Kleinen, Thomas Brovkin, Victor |
spellingShingle |
de Vrese, Philipp Stacke, Tobias Kleinen, Thomas Brovkin, Victor Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
author_facet |
de Vrese, Philipp Stacke, Tobias Kleinen, Thomas Brovkin, Victor |
author_sort |
de Vrese, Philipp |
title |
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
title_short |
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
title_full |
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
title_fullStr |
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
title_full_unstemmed |
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios |
title_sort |
diverging responses of high-latitude co2 and ch4 emissions in idealized climate change scenarios |
publisher |
Copernicus Publications (EGU) |
publishDate |
2021 |
url |
https://oceanrep.geomar.de/id/eprint/52534/ https://oceanrep.geomar.de/id/eprint/52534/1/tc-15-1097-2021.pdf https://doi.org/10.5194/tc-15-1097-2021 |
genre |
permafrost The Cryosphere |
genre_facet |
permafrost The Cryosphere |
op_relation |
https://oceanrep.geomar.de/id/eprint/52534/1/tc-15-1097-2021.pdf de Vrese, P., Stacke, T., Kleinen, T. and Brovkin, V. (2021) Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios. Open Access The Cryosphere, 15 (2). pp. 1097-1130. DOI 10.5194/tc-15-1097-2021 <https://doi.org/10.5194/tc-15-1097-2021>. doi:10.5194/tc-15-1097-2021 |
op_rights |
cc_by_4.0 info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-15-1097-2021 |
container_title |
The Cryosphere |
container_volume |
15 |
container_issue |
2 |
container_start_page |
1097 |
op_container_end_page |
1130 |
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