High-resolution regional simulation of last glacial maximum climate in Europe
A fully coupled atmosphere–ocean general circulation model is used to simulate climate conditions during the last glacial maximum (LGM). Forcing conditions include astronomical parameters, greenhouse gases, ice sheets and vegetation. A 50-yr period of the global simulation is dynamically downscaled...
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Online Access: | https://doi.org/10.1111/j.1600-0870.2010.00485.x http://handle.westernsydney.edu.au:8081/1959.7/uws:48427 |
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ftunivwestsyd:oai:researchdirect.westernsydney.edu.au:uws_48427 2023-05-15T16:40:18+02:00 High-resolution regional simulation of last glacial maximum climate in Europe Strandberg, Gustav Brandefelt, Jenny Kjellstrom, Erik Smith, Benjamin (R19508) Hawkesbury Institute for the Environment (Host institution) 2011 print 19 https://doi.org/10.1111/j.1600-0870.2010.00485.x http://handle.westernsydney.edu.au:8081/1959.7/uws:48427 eng eng Sweden, Co-Action Publishing Tellus Series A: Dynamic Meteorology and Oceanography--1600-0870--0280-6495 Vol. 63 Issue. 1 No. pp: 107-125 XXXXXX - Unknown Last Glacial Maximum computer simulation Europe journal article 2011 ftunivwestsyd https://doi.org/10.1111/j.1600-0870.2010.00485.x 2020-12-05T17:54:44Z A fully coupled atmosphere–ocean general circulation model is used to simulate climate conditions during the last glacial maximum (LGM). Forcing conditions include astronomical parameters, greenhouse gases, ice sheets and vegetation. A 50-yr period of the global simulation is dynamically downscaled to 50 km horizontal resolution over Europe with a regional climate model (RCM). A dynamic vegetation model is used to produce vegetation that is consistent with the climate simulated by the RCM. This vegetation is used in a final simulation with the RCM. The resulting climate is 5–10 ◦C colder than the recent past climate (representative of year 1990) over ice-free parts of Europe as an annual average; over the ice-sheet up to 40 ◦C colder in winter. The average model-proxy error is about the same for summer and winter, for pollen-based proxies. The RCM results are within (outside) the uncertainty limits for winter (summer). Sensitivity studies performed with the RCM indicate that the simulated climate is sensitive to changes in vegetation, whereas the location of the ice sheet only affects the climate around the ice sheet. The RCM-simulated interannual variability in near surface temperature is significantly larger at LGM than in the recent past climate. Article in Journal/Newspaper Ice Sheet University of Western Sydney (UWS): Research Direct Tellus A: Dynamic Meteorology and Oceanography 63 1 107 125 |
institution |
Open Polar |
collection |
University of Western Sydney (UWS): Research Direct |
op_collection_id |
ftunivwestsyd |
language |
English |
topic |
XXXXXX - Unknown Last Glacial Maximum computer simulation Europe |
spellingShingle |
XXXXXX - Unknown Last Glacial Maximum computer simulation Europe Strandberg, Gustav Brandefelt, Jenny Kjellstrom, Erik Smith, Benjamin (R19508) High-resolution regional simulation of last glacial maximum climate in Europe |
topic_facet |
XXXXXX - Unknown Last Glacial Maximum computer simulation Europe |
description |
A fully coupled atmosphere–ocean general circulation model is used to simulate climate conditions during the last glacial maximum (LGM). Forcing conditions include astronomical parameters, greenhouse gases, ice sheets and vegetation. A 50-yr period of the global simulation is dynamically downscaled to 50 km horizontal resolution over Europe with a regional climate model (RCM). A dynamic vegetation model is used to produce vegetation that is consistent with the climate simulated by the RCM. This vegetation is used in a final simulation with the RCM. The resulting climate is 5–10 ◦C colder than the recent past climate (representative of year 1990) over ice-free parts of Europe as an annual average; over the ice-sheet up to 40 ◦C colder in winter. The average model-proxy error is about the same for summer and winter, for pollen-based proxies. The RCM results are within (outside) the uncertainty limits for winter (summer). Sensitivity studies performed with the RCM indicate that the simulated climate is sensitive to changes in vegetation, whereas the location of the ice sheet only affects the climate around the ice sheet. The RCM-simulated interannual variability in near surface temperature is significantly larger at LGM than in the recent past climate. |
author2 |
Hawkesbury Institute for the Environment (Host institution) |
format |
Article in Journal/Newspaper |
author |
Strandberg, Gustav Brandefelt, Jenny Kjellstrom, Erik Smith, Benjamin (R19508) |
author_facet |
Strandberg, Gustav Brandefelt, Jenny Kjellstrom, Erik Smith, Benjamin (R19508) |
author_sort |
Strandberg, Gustav |
title |
High-resolution regional simulation of last glacial maximum climate in Europe |
title_short |
High-resolution regional simulation of last glacial maximum climate in Europe |
title_full |
High-resolution regional simulation of last glacial maximum climate in Europe |
title_fullStr |
High-resolution regional simulation of last glacial maximum climate in Europe |
title_full_unstemmed |
High-resolution regional simulation of last glacial maximum climate in Europe |
title_sort |
high-resolution regional simulation of last glacial maximum climate in europe |
publisher |
Sweden, Co-Action Publishing |
publishDate |
2011 |
url |
https://doi.org/10.1111/j.1600-0870.2010.00485.x http://handle.westernsydney.edu.au:8081/1959.7/uws:48427 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Tellus Series A: Dynamic Meteorology and Oceanography--1600-0870--0280-6495 Vol. 63 Issue. 1 No. pp: 107-125 |
op_doi |
https://doi.org/10.1111/j.1600-0870.2010.00485.x |
container_title |
Tellus A: Dynamic Meteorology and Oceanography |
container_volume |
63 |
container_issue |
1 |
container_start_page |
107 |
op_container_end_page |
125 |
_version_ |
1766030682887290880 |