Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis
Abstract The sensitivity of the last glacial-inception (around 115 kyr BP, 115,000 years before present) to different feedback mechanisms has been analysed by using the Earth system model of intermediate complexity CLIMBER-2. CLIMBER-2 includes dynamic modules of the atmosphere, ocean, terrestrial b...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.1070.8092 2023-05-15T16:41:23+02:00 Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis Reinhard Calov A E Andrey Ganopolski Ae Vladimir Petoukhov Martin Claussen A E Victor Brovkin Ae Claudia Kubatzki The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.8092 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.8092 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf text 2005 ftciteseerx 2020-04-26T00:21:31Z Abstract The sensitivity of the last glacial-inception (around 115 kyr BP, 115,000 years before present) to different feedback mechanisms has been analysed by using the Earth system model of intermediate complexity CLIMBER-2. CLIMBER-2 includes dynamic modules of the atmosphere, ocean, terrestrial biosphere and inland ice, the last of which was added recently by utilising the three-dimensonal polythermal ice-sheet model SICOPOLIS. We performed a set of transient experiments starting at the middle of the Eemiam interglacial and ran the model for 26,000 years with time-dependent orbital forcing and observed changes in atmospheric CO 2 concentration (CO 2 forcing). The role of vegetation and ocean feedback, CO 2 forcing, mineral dust, thermohaline circulation and orbital insolation were closely investigated. In our model, glacial inception, as a bifurcation in the climate system, appears in nearly all sensitivity runs including a run with constant atmospheric CO 2 concentration of 280 ppmv, a typical interglacial value, and simulations with prescribed present-day sea-surface temperatures or vegetation cover-although the rate of the growth of ice-sheets growth is smaller than in the case of the fully interactive model. Only if we run the fully interactive model with constant present-day insolation and apply present-day CO 2 forcing does no glacial inception appear at all. This implies that, within our model, the orbital forcing alone is sufficient to trigger the interglacial-glacial transition, while vegetation, ocean and atmospheric CO 2 concentration only provide additional, although important, positive feedbacks. In addition, we found that possible reorganisations of the thermohaline circulation influence the distribution of inland ice. Text Ice Sheet Unknown |
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Abstract The sensitivity of the last glacial-inception (around 115 kyr BP, 115,000 years before present) to different feedback mechanisms has been analysed by using the Earth system model of intermediate complexity CLIMBER-2. CLIMBER-2 includes dynamic modules of the atmosphere, ocean, terrestrial biosphere and inland ice, the last of which was added recently by utilising the three-dimensonal polythermal ice-sheet model SICOPOLIS. We performed a set of transient experiments starting at the middle of the Eemiam interglacial and ran the model for 26,000 years with time-dependent orbital forcing and observed changes in atmospheric CO 2 concentration (CO 2 forcing). The role of vegetation and ocean feedback, CO 2 forcing, mineral dust, thermohaline circulation and orbital insolation were closely investigated. In our model, glacial inception, as a bifurcation in the climate system, appears in nearly all sensitivity runs including a run with constant atmospheric CO 2 concentration of 280 ppmv, a typical interglacial value, and simulations with prescribed present-day sea-surface temperatures or vegetation cover-although the rate of the growth of ice-sheets growth is smaller than in the case of the fully interactive model. Only if we run the fully interactive model with constant present-day insolation and apply present-day CO 2 forcing does no glacial inception appear at all. This implies that, within our model, the orbital forcing alone is sufficient to trigger the interglacial-glacial transition, while vegetation, ocean and atmospheric CO 2 concentration only provide additional, although important, positive feedbacks. In addition, we found that possible reorganisations of the thermohaline circulation influence the distribution of inland ice. |
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The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Reinhard Calov A E Andrey Ganopolski Ae Vladimir Petoukhov Martin Claussen A E Victor Brovkin Ae Claudia Kubatzki |
spellingShingle |
Reinhard Calov A E Andrey Ganopolski Ae Vladimir Petoukhov Martin Claussen A E Victor Brovkin Ae Claudia Kubatzki Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
author_facet |
Reinhard Calov A E Andrey Ganopolski Ae Vladimir Petoukhov Martin Claussen A E Victor Brovkin Ae Claudia Kubatzki |
author_sort |
Reinhard Calov |
title |
Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
title_short |
Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
title_full |
Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
title_fullStr |
Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
title_full_unstemmed |
Transient simulation of the last glacial inception. Part II: sensitivity and feedback analysis |
title_sort |
transient simulation of the last glacial inception. part ii: sensitivity and feedback analysis |
publishDate |
2005 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.8092 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.8092 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/calov_al_glac-incep-2_climdyn_05.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766031809327398912 |