Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6

Abstract We investigate the sensitivity of simulations of the last glacial inception (LGI) with respect to initial (size of the Greenland ice sheet) and surface (state of ocean/vegetation) conditions and two different CO2 reconstructions. Utilizing the CLIMBER-2 Earth system model, we obtain the fol...

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Main Authors: Claudia Kubatzki, Æ Martin Claussen, Æ Reinhard Calov, Andrey Ganopolski, C. Kubatzki, Present Address M. Claussen
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.7585
http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/kubatzki_al_incep_climdyn06.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.362.7585 2023-05-15T16:26:06+02:00 Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6 Claudia Kubatzki Æ Martin Claussen Æ Reinhard Calov Andrey Ganopolski C. Kubatzki Present Address M. Claussen The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.7585 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/kubatzki_al_incep_climdyn06.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.7585 http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/kubatzki_al_incep_climdyn06.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/kubatzki_al_incep_climdyn06.pdf text 2005 ftciteseerx 2016-01-08T00:54:36Z Abstract We investigate the sensitivity of simulations of the last glacial inception (LGI) with respect to initial (size of the Greenland ice sheet) and surface (state of ocean/vegetation) conditions and two different CO2 reconstructions. Utilizing the CLIMBER-2 Earth system model, we obtain the following results: (a) ice-sheet expansion in North America at the end of the Eemian can be reduced or even completely suppressed when pre-industrial or Eemian ocean/vegetation is prescribed. (b) A warmer surrounding ocean and, in particular, a large Laurentide ice sheet reduce the size of the Greenland ice sheet before and during the LGI. (c) A changing ocean contributes much stronger to the expansion of the Laurentide ice sheet when we apply the CO2 reconstruction according to Barnola et al. (Nature 329:408–414, 1987) instead of Petit et al. (Nature 399:429– 436, 1999). (d) In the fully coupled model, the CO2 reconstruction used has only a small impact on the simulated ice sheets but it does impact the course of the climatic variables. (e) For the Greenland ice sheet, two equilibrium states exist under the insolation and CO2 forcing at 128,000 years before present (128 kyear BP); the one with an ice sheet reduced by about one quarter as compared to its simulated pre-industrial size and the other with nearly no inland ice in Greenland. (f) Even the extreme assumption of no ice sheet in Greenland at the beginning of our transient simulations does not alter the simulated expansion of northern hemispheric ice sheets at the LGI. Text Greenland Ice Sheet Unknown Greenland
institution Open Polar
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description Abstract We investigate the sensitivity of simulations of the last glacial inception (LGI) with respect to initial (size of the Greenland ice sheet) and surface (state of ocean/vegetation) conditions and two different CO2 reconstructions. Utilizing the CLIMBER-2 Earth system model, we obtain the following results: (a) ice-sheet expansion in North America at the end of the Eemian can be reduced or even completely suppressed when pre-industrial or Eemian ocean/vegetation is prescribed. (b) A warmer surrounding ocean and, in particular, a large Laurentide ice sheet reduce the size of the Greenland ice sheet before and during the LGI. (c) A changing ocean contributes much stronger to the expansion of the Laurentide ice sheet when we apply the CO2 reconstruction according to Barnola et al. (Nature 329:408–414, 1987) instead of Petit et al. (Nature 399:429– 436, 1999). (d) In the fully coupled model, the CO2 reconstruction used has only a small impact on the simulated ice sheets but it does impact the course of the climatic variables. (e) For the Greenland ice sheet, two equilibrium states exist under the insolation and CO2 forcing at 128,000 years before present (128 kyear BP); the one with an ice sheet reduced by about one quarter as compared to its simulated pre-industrial size and the other with nearly no inland ice in Greenland. (f) Even the extreme assumption of no ice sheet in Greenland at the beginning of our transient simulations does not alter the simulated expansion of northern hemispheric ice sheets at the LGI.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Claudia Kubatzki
Æ Martin Claussen
Æ Reinhard Calov
Andrey Ganopolski
C. Kubatzki
Present Address M. Claussen
spellingShingle Claudia Kubatzki
Æ Martin Claussen
Æ Reinhard Calov
Andrey Ganopolski
C. Kubatzki
Present Address M. Claussen
Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
author_facet Claudia Kubatzki
Æ Martin Claussen
Æ Reinhard Calov
Andrey Ganopolski
C. Kubatzki
Present Address M. Claussen
author_sort Claudia Kubatzki
title Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
title_short Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
title_full Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
title_fullStr Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
title_full_unstemmed Climate Dynamics (2006) DOI 10.1007/s00382-006-0136-6
title_sort climate dynamics (2006) doi 10.1007/s00382-006-0136-6
publishDate 2005
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.362.7585
http://www.mpimet.mpg.de/fileadmin/staff/claussenmartin/publications/kubatzki_al_incep_climdyn06.pdf
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
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