Atmospheric CO2 response to AMOC changes under high and low obliquity ...
Meltwater experiments are performed with the Earth system model of intermediate complexity LOVECLIM (Goosse et al., 2010) under 49ka and 12 ka boundary conditions with their appropriate obliquity values as well as with low obliquity (22.1 deg). The impact on atmospheric CO2 and the oceanic and terre...
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UNSW Sydney
2024
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Online Access: | https://dx.doi.org/10.26190/unsworks/30408 http://hdl.handle.net/1959.4/102810 |
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ftdatacite:10.26190/unsworks/30408 2024-09-30T14:26:53+00:00 Atmospheric CO2 response to AMOC changes under high and low obliquity ... Menviel, Laurie 2024 https://dx.doi.org/10.26190/unsworks/30408 http://hdl.handle.net/1959.4/102810 en eng UNSW Sydney Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 AMOC Carbon cycle Orbital parameters 370201 Climate change processes 370203 Greenhouse gas inventories and fluxes 190501 Climate change models 190507 Global effects of climate change excl. Australia, New Zealand, Antarctica and the South Pacific excl. social impacts Dataset dataset 2024 ftdatacite https://doi.org/10.26190/unsworks/30408 2024-09-02T09:11:06Z Meltwater experiments are performed with the Earth system model of intermediate complexity LOVECLIM (Goosse et al., 2010) under 49ka and 12 ka boundary conditions with their appropriate obliquity values as well as with low obliquity (22.1 deg). The impact on atmospheric CO2 and the oceanic and terrestrial carbon cycle is assessed to understand the impact of obliquity on the carbon cycle. Details on the scientific context and experimental design are in Legrain E., Capron E., Menviel, L. et al., "Centennial-scale variations in the carbon cycle enhanced by high obliquity", 2024. ... : The Earth system model of intermediate complexity LOVECLIM (Goosse et al., 2010) is spined up under 49ka and 12 ka boundary conditions (ice-sheet geometry and albedo (Abe-Ouchi et al., 2013), orbital parameters (Berger et al,, 1978)) with prognostic atmospheric CO2. These spinups are branched from transient simulations of the last interglacial-glacial cycle performed with LOVECLIM, so that the initial conditions of these spinups also have appropriate greenhouse gas forcing (Koehler et al., 2017). Two other control experiments are performed. They are similar to the 49ka and 12ka control, but have a low obliquity of 22.1 degrees. From these 4 control states, freshwater is added into the North Atlantic (60W-10°W, 50N-60°N) at a rate of 0.3 Sv for the 49ka experiments and 0.16 Sv for the 12ka experiments. ... Dataset Antarc* Antarctica Ice Sheet North Atlantic DataCite New Zealand Pacific |
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language |
English |
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AMOC Carbon cycle Orbital parameters 370201 Climate change processes 370203 Greenhouse gas inventories and fluxes 190501 Climate change models 190507 Global effects of climate change excl. Australia, New Zealand, Antarctica and the South Pacific excl. social impacts |
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AMOC Carbon cycle Orbital parameters 370201 Climate change processes 370203 Greenhouse gas inventories and fluxes 190501 Climate change models 190507 Global effects of climate change excl. Australia, New Zealand, Antarctica and the South Pacific excl. social impacts Menviel, Laurie Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
topic_facet |
AMOC Carbon cycle Orbital parameters 370201 Climate change processes 370203 Greenhouse gas inventories and fluxes 190501 Climate change models 190507 Global effects of climate change excl. Australia, New Zealand, Antarctica and the South Pacific excl. social impacts |
description |
Meltwater experiments are performed with the Earth system model of intermediate complexity LOVECLIM (Goosse et al., 2010) under 49ka and 12 ka boundary conditions with their appropriate obliquity values as well as with low obliquity (22.1 deg). The impact on atmospheric CO2 and the oceanic and terrestrial carbon cycle is assessed to understand the impact of obliquity on the carbon cycle. Details on the scientific context and experimental design are in Legrain E., Capron E., Menviel, L. et al., "Centennial-scale variations in the carbon cycle enhanced by high obliquity", 2024. ... : The Earth system model of intermediate complexity LOVECLIM (Goosse et al., 2010) is spined up under 49ka and 12 ka boundary conditions (ice-sheet geometry and albedo (Abe-Ouchi et al., 2013), orbital parameters (Berger et al,, 1978)) with prognostic atmospheric CO2. These spinups are branched from transient simulations of the last interglacial-glacial cycle performed with LOVECLIM, so that the initial conditions of these spinups also have appropriate greenhouse gas forcing (Koehler et al., 2017). Two other control experiments are performed. They are similar to the 49ka and 12ka control, but have a low obliquity of 22.1 degrees. From these 4 control states, freshwater is added into the North Atlantic (60W-10°W, 50N-60°N) at a rate of 0.3 Sv for the 49ka experiments and 0.16 Sv for the 12ka experiments. ... |
format |
Dataset |
author |
Menviel, Laurie |
author_facet |
Menviel, Laurie |
author_sort |
Menviel, Laurie |
title |
Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
title_short |
Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
title_full |
Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
title_fullStr |
Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
title_full_unstemmed |
Atmospheric CO2 response to AMOC changes under high and low obliquity ... |
title_sort |
atmospheric co2 response to amoc changes under high and low obliquity ... |
publisher |
UNSW Sydney |
publishDate |
2024 |
url |
https://dx.doi.org/10.26190/unsworks/30408 http://hdl.handle.net/1959.4/102810 |
geographic |
New Zealand Pacific |
geographic_facet |
New Zealand Pacific |
genre |
Antarc* Antarctica Ice Sheet North Atlantic |
genre_facet |
Antarc* Antarctica Ice Sheet North Atlantic |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.26190/unsworks/30408 |
_version_ |
1811633006470758400 |