A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling

The canonical question of which physical, chemical or biological mechanisms were responsible for oceanic uptake of atmospheric CO 2 during the last glacial is yet unanswered. Insight from paleo proxies has led to a multitude of hypotheses but none so far have been convincingly supported in three dim...

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Main Authors: de Boer, A. M., Watson, A. J., Edwards, N. R., Oliver, K. I. C.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2010
Subjects:
Online Access:https://oro.open.ac.uk/25666/
https://oro.open.ac.uk/25666/1/DeBoer_etal_CP_10.pdf
https://doi.org/10.5194/cpd-6-867-2010
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spelling ftopenunivgb:oai:oro.open.ac.uk:25666 2023-06-11T04:05:49+02:00 A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling de Boer, A. M. Watson, A. J. Edwards, N. R. Oliver, K. I. C. 2010 application/pdf https://oro.open.ac.uk/25666/ https://oro.open.ac.uk/25666/1/DeBoer_etal_CP_10.pdf https://doi.org/10.5194/cpd-6-867-2010 unknown https://oro.open.ac.uk/25666/1/DeBoer_etal_CP_10.pdf de Boer, A. M.; Watson, A. J.; Edwards, N. R. <http://oro.open.ac.uk/view/person/nre29.html> and Oliver, K. I. C. (2010). A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling. Climate of the Past, 6, pp. 867–903. Journal Item Public PeerReviewed 2010 ftopenunivgb https://doi.org/10.5194/cpd-6-867-2010 2023-05-28T05:45:25Z The canonical question of which physical, chemical or biological mechanisms were responsible for oceanic uptake of atmospheric CO 2 during the last glacial is yet unanswered. Insight from paleo proxies has led to a multitude of hypotheses but none so far have been convincingly supported in three dimensional numerical modelling experiments. The processes that influence the CO 2 uptake and export production are inter-related and too complex to solve conceptually while complex numerical models are time consuming and expensive to run which severely limits the combinations of mechanisms that can be explored. Instead, an intermediate inverse box model approach is used here in which the whole parameter space is explored. The glacial circulation and biological production states are derived from these using proxies of glacial export production and the need to draw down CO 2 into the ocean. We find that circulation patterns which explain glacial observations include reduced Antarctic Bottom Water formation and high latitude mixing and to a lesser extent reduced equatorial upwelling. The proposed mechanism of CO 2 uptake by an increase of eddies in the Southern Ocean, leading to a reduced residual circulation, is not supported. Regarding biological mechanisms, an increase in the nutrient utilization in either the equatorial regions or the northern polar latitudes can reduce atmospheric CO 2 and satisfy proxies of glacial export production. Consistent with previous studies, CO 2 is drawn down more easily through increased productivity in the Antarctic region than the sub-Antarctic, but that violates observations of lower export production there. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean The Open University: Open Research Online (ORO) Antarctic Southern Ocean The Antarctic
institution Open Polar
collection The Open University: Open Research Online (ORO)
op_collection_id ftopenunivgb
language unknown
description The canonical question of which physical, chemical or biological mechanisms were responsible for oceanic uptake of atmospheric CO 2 during the last glacial is yet unanswered. Insight from paleo proxies has led to a multitude of hypotheses but none so far have been convincingly supported in three dimensional numerical modelling experiments. The processes that influence the CO 2 uptake and export production are inter-related and too complex to solve conceptually while complex numerical models are time consuming and expensive to run which severely limits the combinations of mechanisms that can be explored. Instead, an intermediate inverse box model approach is used here in which the whole parameter space is explored. The glacial circulation and biological production states are derived from these using proxies of glacial export production and the need to draw down CO 2 into the ocean. We find that circulation patterns which explain glacial observations include reduced Antarctic Bottom Water formation and high latitude mixing and to a lesser extent reduced equatorial upwelling. The proposed mechanism of CO 2 uptake by an increase of eddies in the Southern Ocean, leading to a reduced residual circulation, is not supported. Regarding biological mechanisms, an increase in the nutrient utilization in either the equatorial regions or the northern polar latitudes can reduce atmospheric CO 2 and satisfy proxies of glacial export production. Consistent with previous studies, CO 2 is drawn down more easily through increased productivity in the Antarctic region than the sub-Antarctic, but that violates observations of lower export production there.
format Article in Journal/Newspaper
author de Boer, A. M.
Watson, A. J.
Edwards, N. R.
Oliver, K. I. C.
spellingShingle de Boer, A. M.
Watson, A. J.
Edwards, N. R.
Oliver, K. I. C.
A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
author_facet de Boer, A. M.
Watson, A. J.
Edwards, N. R.
Oliver, K. I. C.
author_sort de Boer, A. M.
title A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
title_short A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
title_full A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
title_fullStr A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
title_full_unstemmed A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
title_sort comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling
publishDate 2010
url https://oro.open.ac.uk/25666/
https://oro.open.ac.uk/25666/1/DeBoer_etal_CP_10.pdf
https://doi.org/10.5194/cpd-6-867-2010
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_relation https://oro.open.ac.uk/25666/1/DeBoer_etal_CP_10.pdf
de Boer, A. M.; Watson, A. J.; Edwards, N. R. <http://oro.open.ac.uk/view/person/nre29.html> and Oliver, K. I. C. (2010). A comprehensive, multi-process box-model approach to glacial-interglacial carbon cycling. Climate of the Past, 6, pp. 867–903.
op_doi https://doi.org/10.5194/cpd-6-867-2010
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