Transient simulation of the last glacial inception, Part II: sensitivity and feedback analysis
We study the mechanisms of glacial inception by using the Earth system model of intermediate complexity CLIMBER-2, which encompasses dynamic modules of the atmosphere, ocean, biosphere and ice sheets. Ice-sheet dynamics are described by the 3-dimensional polythermal ice-sheet model SICOPOLIS. We hav...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.464.286 2023-05-15T16:40:33+02:00 Transient simulation of the last glacial inception, Part II: sensitivity and feedback analysis Reinhard Calov Andrey Ganopolski Martin Claussen Vladimir Petoukhov Ralf Greve The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.286 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.286 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf text 2005 ftciteseerx 2016-01-08T06:48:40Z We study the mechanisms of glacial inception by using the Earth system model of intermediate complexity CLIMBER-2, which encompasses dynamic modules of the atmosphere, ocean, biosphere and ice sheets. Ice-sheet dynamics are described by the 3-dimensional polythermal ice-sheet model SICOPOLIS. We have performed transient experiments starting at the Eemiam interglacial, at 126 kyr BP (126,000 years before present). The model runs for 26,000 years with time-dependent orbital and CO2 forcings. The model simulates a rapid expansion of the area covered by inland ice in the Northern Hemisphere, predominantly over Northern America, starting at about 117 kyr BP. During the next 7 kyr, the ice volume grows gradually in the model at a rate which corresponds to a change in sea level of 10 m per millennium. We have shown that the simulated glacial inception represents a bifurcation transition in the climate system from an interglacial to a glacial state caused by the strong snow-albedo feedback. This transition occurs when summer insolation at high latitudes of the Northern Hemisphere drops below a threshold value, which is only slightly lower than modern summer insolation. By performing long-term equilibrium runs, we find that for the present-day orbital parameters at least two Text Ice Sheet Unknown |
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ftciteseerx |
language |
English |
description |
We study the mechanisms of glacial inception by using the Earth system model of intermediate complexity CLIMBER-2, which encompasses dynamic modules of the atmosphere, ocean, biosphere and ice sheets. Ice-sheet dynamics are described by the 3-dimensional polythermal ice-sheet model SICOPOLIS. We have performed transient experiments starting at the Eemiam interglacial, at 126 kyr BP (126,000 years before present). The model runs for 26,000 years with time-dependent orbital and CO2 forcings. The model simulates a rapid expansion of the area covered by inland ice in the Northern Hemisphere, predominantly over Northern America, starting at about 117 kyr BP. During the next 7 kyr, the ice volume grows gradually in the model at a rate which corresponds to a change in sea level of 10 m per millennium. We have shown that the simulated glacial inception represents a bifurcation transition in the climate system from an interglacial to a glacial state caused by the strong snow-albedo feedback. This transition occurs when summer insolation at high latitudes of the Northern Hemisphere drops below a threshold value, which is only slightly lower than modern summer insolation. By performing long-term equilibrium runs, we find that for the present-day orbital parameters at least two |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Reinhard Calov Andrey Ganopolski Martin Claussen Vladimir Petoukhov Ralf Greve |
spellingShingle |
Reinhard Calov Andrey Ganopolski Martin Claussen Vladimir Petoukhov Ralf Greve Transient simulation of the last glacial inception, Part II: sensitivity and feedback analysis |
author_facet |
Reinhard Calov Andrey Ganopolski Martin Claussen Vladimir Petoukhov Ralf Greve |
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=10.1.1.464.286 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_source |
http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.464.286 http://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/29692/1/CD24-6.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766030951355252736 |