Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies?
Most state-of-the-art climate models include a coarsely resolved oceanic component, which hardly captures detailed dynamics, whereas eddy-permitting and eddy-resolving simulations are developed to reproduce the observed ocean. In this study, an eddy-permitting and a coarse resolution numerical exper...
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Copernicus Publications
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Online Access: | https://doi.org/10.5194/cp-9-2669-2013 http://www.clim-past.net/9/2669/2013/cp-9-2669-2013.pdf https://doaj.org/article/61a972f0483c4fc787d8656f324f0aed |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:61a972f0483c4fc787d8656f324f0aed 2023-05-15T18:18:12+02:00 Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? M. Ballarotta L. Brodeau J. Brandefelt P. Lundberg K. Döös 2013-11-01 https://doi.org/10.5194/cp-9-2669-2013 http://www.clim-past.net/9/2669/2013/cp-9-2669-2013.pdf https://doaj.org/article/61a972f0483c4fc787d8656f324f0aed en eng Copernicus Publications 1814-9324 1814-9332 doi:10.5194/cp-9-2669-2013 http://www.clim-past.net/9/2669/2013/cp-9-2669-2013.pdf https://doaj.org/article/61a972f0483c4fc787d8656f324f0aed undefined Climate of the Past, Vol 9, Iss 6, Pp 2669-2686 (2013) envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2013 fttriple https://doi.org/10.5194/cp-9-2669-2013 2023-01-22T17:58:07Z Most state-of-the-art climate models include a coarsely resolved oceanic component, which hardly captures detailed dynamics, whereas eddy-permitting and eddy-resolving simulations are developed to reproduce the observed ocean. In this study, an eddy-permitting and a coarse resolution numerical experiment are conducted to simulate the global ocean state for the period of the Last Glacial Maximum (LGM, ~26 500 to 19 000 yr ago) and to investigate the improvements due to taking into account the smaller spatial scales. The ocean state from each simulation is confronted with a data set from the Multiproxy Approach for the Reconstruction of the Glacial Ocean (MARGO) sea surface temperatures (SSTs), some reconstructions of the palaeo-circulations and a number of sea-ice reconstructions. The western boundary currents and the Southern Ocean dynamics are better resolved in the high-resolution experiment than in the coarse simulation, but, although these more detailed SST structures yield a locally improved consistency between model predictions and proxies, they do not contribute significantly to the global statistical score. The SSTs in the tropical coastal upwelling zones are also not significantly improved by the eddy-permitting regime. The models perform in the mid-latitudes but as in the majority of the Paleoclimate Modelling Intercomparison Project simulations, the modelled sea-ice conditions are inconsistent with the palaeo-reconstructions. The effects of observation locations on the comparison between observed and simulated SST suggest that more sediment cores may be required to draw reliable conclusions about the improvements introduced by the high resolution model for reproducing the global SSTs. One has to be careful with the interpretation of the deep ocean state which has not reached statistical equilibrium in our simulations. However, the results indicate that the meridional overturning circulations are different between the two regimes, suggesting that the model parametrizations might also play a key role ... Article in Journal/Newspaper Sea ice Southern Ocean Unknown Southern Ocean Climate of the Past 9 6 2669 2686 |
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English |
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envir geo |
spellingShingle |
envir geo M. Ballarotta L. Brodeau J. Brandefelt P. Lundberg K. Döös Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
topic_facet |
envir geo |
description |
Most state-of-the-art climate models include a coarsely resolved oceanic component, which hardly captures detailed dynamics, whereas eddy-permitting and eddy-resolving simulations are developed to reproduce the observed ocean. In this study, an eddy-permitting and a coarse resolution numerical experiment are conducted to simulate the global ocean state for the period of the Last Glacial Maximum (LGM, ~26 500 to 19 000 yr ago) and to investigate the improvements due to taking into account the smaller spatial scales. The ocean state from each simulation is confronted with a data set from the Multiproxy Approach for the Reconstruction of the Glacial Ocean (MARGO) sea surface temperatures (SSTs), some reconstructions of the palaeo-circulations and a number of sea-ice reconstructions. The western boundary currents and the Southern Ocean dynamics are better resolved in the high-resolution experiment than in the coarse simulation, but, although these more detailed SST structures yield a locally improved consistency between model predictions and proxies, they do not contribute significantly to the global statistical score. The SSTs in the tropical coastal upwelling zones are also not significantly improved by the eddy-permitting regime. The models perform in the mid-latitudes but as in the majority of the Paleoclimate Modelling Intercomparison Project simulations, the modelled sea-ice conditions are inconsistent with the palaeo-reconstructions. The effects of observation locations on the comparison between observed and simulated SST suggest that more sediment cores may be required to draw reliable conclusions about the improvements introduced by the high resolution model for reproducing the global SSTs. One has to be careful with the interpretation of the deep ocean state which has not reached statistical equilibrium in our simulations. However, the results indicate that the meridional overturning circulations are different between the two regimes, suggesting that the model parametrizations might also play a key role ... |
format |
Article in Journal/Newspaper |
author |
M. Ballarotta L. Brodeau J. Brandefelt P. Lundberg K. Döös |
author_facet |
M. Ballarotta L. Brodeau J. Brandefelt P. Lundberg K. Döös |
author_sort |
M. Ballarotta |
title |
Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
title_short |
Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
title_full |
Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
title_fullStr |
Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
title_full_unstemmed |
Last Glacial Maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
title_sort |
last glacial maximum world ocean simulations at eddy-permitting and coarse resolutions: do eddies contribute to a better consistency between models and palaeoproxies? |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/cp-9-2669-2013 http://www.clim-past.net/9/2669/2013/cp-9-2669-2013.pdf https://doaj.org/article/61a972f0483c4fc787d8656f324f0aed |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Sea ice Southern Ocean |
genre_facet |
Sea ice Southern Ocean |
op_source |
Climate of the Past, Vol 9, Iss 6, Pp 2669-2686 (2013) |
op_relation |
1814-9324 1814-9332 doi:10.5194/cp-9-2669-2013 http://www.clim-past.net/9/2669/2013/cp-9-2669-2013.pdf https://doaj.org/article/61a972f0483c4fc787d8656f324f0aed |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/cp-9-2669-2013 |
container_title |
Climate of the Past |
container_volume |
9 |
container_issue |
6 |
container_start_page |
2669 |
op_container_end_page |
2686 |
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