No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2

The relative impact of the CO2 concentration on climate-over the last 200 kyr is investigated here using the Louvain-la-Neuve 2-dimension Northern Hemisphere (LLN 2-D NH) climate model forced by different constant insolations and the variable CO2 concentration reconstructed from the Vostok ice-core...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Loutre, Marie-France, Berger, André
Other Authors: UCL - SC/PHYS - Département de physique
Format: Article in Journal/Newspaper
Language:English
Published: Amer Geophysical Union 2000
Subjects:
Online Access:http://hdl.handle.net/2078.1/43665
https://doi.org/10.1029/1999GL006081
id ftunistlouisbrus:oai:dial.uclouvain.be:boreal:43665
record_format openpolar
spelling ftunistlouisbrus:oai:dial.uclouvain.be:boreal:43665 2024-05-12T08:05:12+00:00 No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2 Loutre, Marie-France Berger, André UCL - SC/PHYS - Département de physique 2000 http://hdl.handle.net/2078.1/43665 https://doi.org/10.1029/1999GL006081 eng eng Amer Geophysical Union boreal:43665 http://hdl.handle.net/2078.1/43665 doi:10.1029/1999GL006081 urn:ISSN:0094-8276 urn:EISSN:1944-8007 Geophysical Research Letters, Vol. 27, no. 6, p. 783-786 (2000) info:eu-repo/semantics/article 2000 ftunistlouisbrus https://doi.org/10.1029/1999GL006081 2024-04-18T18:14:15Z The relative impact of the CO2 concentration on climate-over the last 200 kyr is investigated here using the Louvain-la-Neuve 2-dimension Northern Hemisphere (LLN 2-D NH) climate model forced by different constant insolations and the variable CO2 concentration reconstructed from the Vostok ice-core record. Under such conditions the 100-kyr cycle in-the Northern Hemisphere ice volume cannot be reproduced. Either a warm orbit prevents the ice sheets from forming-or a present-day and colder orbits do not allow them tol:melt:after being formed. The global hemispheric temperature,, however, continues to respond directly to the atmospheric CO2-concentration changes. Article in Journal/Newspaper ice core DIAL@USL-B (Université Saint-Louis, Bruxelles) Geophysical Research Letters 27 6 783 786
institution Open Polar
collection DIAL@USL-B (Université Saint-Louis, Bruxelles)
op_collection_id ftunistlouisbrus
language English
description The relative impact of the CO2 concentration on climate-over the last 200 kyr is investigated here using the Louvain-la-Neuve 2-dimension Northern Hemisphere (LLN 2-D NH) climate model forced by different constant insolations and the variable CO2 concentration reconstructed from the Vostok ice-core record. Under such conditions the 100-kyr cycle in-the Northern Hemisphere ice volume cannot be reproduced. Either a warm orbit prevents the ice sheets from forming-or a present-day and colder orbits do not allow them tol:melt:after being formed. The global hemispheric temperature,, however, continues to respond directly to the atmospheric CO2-concentration changes.
author2 UCL - SC/PHYS - Département de physique
format Article in Journal/Newspaper
author Loutre, Marie-France
Berger, André
spellingShingle Loutre, Marie-France
Berger, André
No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
author_facet Loutre, Marie-France
Berger, André
author_sort Loutre, Marie-France
title No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
title_short No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
title_full No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
title_fullStr No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
title_full_unstemmed No glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable CO2
title_sort no glacial-interglacial cycle in the ice volume simulated under a constant astronomical forcing and a variable co2
publisher Amer Geophysical Union
publishDate 2000
url http://hdl.handle.net/2078.1/43665
https://doi.org/10.1029/1999GL006081
genre ice core
genre_facet ice core
op_source Geophysical Research Letters, Vol. 27, no. 6, p. 783-786 (2000)
op_relation boreal:43665
http://hdl.handle.net/2078.1/43665
doi:10.1029/1999GL006081
urn:ISSN:0094-8276
urn:EISSN:1944-8007
op_doi https://doi.org/10.1029/1999GL006081
container_title Geophysical Research Letters
container_volume 27
container_issue 6
container_start_page 783
op_container_end_page 786
_version_ 1798847462162563072