Transient changes in the global carbon cycle
The global carbon cycle plays a significant role in glacial/interglacial transitions. On one hand because carbon reservoirs and exchange rates are subject to external climate conditions, on the other hand because changes in carbon dioxide concentrations lead to amplification and mediation of regiona...
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ftawi:oai:epic.awi.de:10530 2023-09-05T13:13:03+02:00 Transient changes in the global carbon cycle Fischer, Hubertus Köhler, Peter 2004 https://epic.awi.de/id/eprint/10530/ https://hdl.handle.net/10013/epic.21007 unknown Fischer, H. and Köhler, P. orcid:0000-0003-0904-8484 (2004) Transient changes in the global carbon cycle , Invited Keynote Lecture. Palaeoclimate: Reducing the uncertainties, 6.-9. July 2004 Utrecht, The Netherlands. . hdl:10013/epic.21007 EPIC3Invited Keynote Lecture. Palaeoclimate: Reducing the uncertainties, 6.-9. July 2004 Utrecht, The Netherlands. Conference notRev 2004 ftawi 2023-08-22T19:48:43Z The global carbon cycle plays a significant role in glacial/interglacial transitions. On one hand because carbon reservoirs and exchange rates are subject to external climate conditions, on the other hand because changes in carbon dioxide concentrations lead to amplification and mediation of regional climate variations.Time slice experiments so far were unable to unambiguously explain the driving forces of the glacial/interglacial change in atmospheric CO2 of about 100 ppmv. Additional information can be gained from the temporal evolution of the carbon cycle using transient model runs, which have to be in line with pronounced variations in ice core CO2 concentrations over the last glacial/interglacial transition.Using a coupled atmosphere/biosphere/ocean box model of the global carbon cycle it is possible to quantify changes in CO2 and d13C observed in Antarctic ice core records. To this end the model is transiently driven by various proxy records over the last 25,000 years. The results show that marine productivity, a breakdown in Southern Ocean stratification triggered by sea ice retreat, the terrestrial biosphere as well as carbonate compensation add at specific intervals to the overall change in CO2 and d13C. Conference Object Antarc* Antarctic ice core Sea ice Southern Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic Southern Ocean |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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The global carbon cycle plays a significant role in glacial/interglacial transitions. On one hand because carbon reservoirs and exchange rates are subject to external climate conditions, on the other hand because changes in carbon dioxide concentrations lead to amplification and mediation of regional climate variations.Time slice experiments so far were unable to unambiguously explain the driving forces of the glacial/interglacial change in atmospheric CO2 of about 100 ppmv. Additional information can be gained from the temporal evolution of the carbon cycle using transient model runs, which have to be in line with pronounced variations in ice core CO2 concentrations over the last glacial/interglacial transition.Using a coupled atmosphere/biosphere/ocean box model of the global carbon cycle it is possible to quantify changes in CO2 and d13C observed in Antarctic ice core records. To this end the model is transiently driven by various proxy records over the last 25,000 years. The results show that marine productivity, a breakdown in Southern Ocean stratification triggered by sea ice retreat, the terrestrial biosphere as well as carbonate compensation add at specific intervals to the overall change in CO2 and d13C. |
format |
Conference Object |
author |
Fischer, Hubertus Köhler, Peter |
spellingShingle |
Fischer, Hubertus Köhler, Peter Transient changes in the global carbon cycle |
author_facet |
Fischer, Hubertus Köhler, Peter |
author_sort |
Fischer, Hubertus |
title |
Transient changes in the global carbon cycle |
title_short |
Transient changes in the global carbon cycle |
title_full |
Transient changes in the global carbon cycle |
title_fullStr |
Transient changes in the global carbon cycle |
title_full_unstemmed |
Transient changes in the global carbon cycle |
title_sort |
transient changes in the global carbon cycle |
publishDate |
2004 |
url |
https://epic.awi.de/id/eprint/10530/ https://hdl.handle.net/10013/epic.21007 |
geographic |
Antarctic Southern Ocean |
geographic_facet |
Antarctic Southern Ocean |
genre |
Antarc* Antarctic ice core Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic ice core Sea ice Southern Ocean |
op_source |
EPIC3Invited Keynote Lecture. Palaeoclimate: Reducing the uncertainties, 6.-9. July 2004 Utrecht, The Netherlands. |
op_relation |
Fischer, H. and Köhler, P. orcid:0000-0003-0904-8484 (2004) Transient changes in the global carbon cycle , Invited Keynote Lecture. Palaeoclimate: Reducing the uncertainties, 6.-9. July 2004 Utrecht, The Netherlands. . hdl:10013/epic.21007 |
_version_ |
1776203211811586048 |