Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry
Interactions between seawater and benthic systems play an important role in global biogeochemical cycling. Benthic fluxes of some chemical elements (e.g., C, N, P, O, Si, Fe, Mn, S) alter the redox state and marine carbonate system (i.e., pH and carbonate saturation state), which in turn modulate th...
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ftnorskinstvf:oai:niva.brage.unit.no:11250/2491308 2023-05-15T17:51:23+02:00 Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry Yakushev, Evgeny Protsenko, Elizaveta Bruggeman, Jorn Wallhead, Philip Pakhomova, Svetlana V. Yakubov, Shamil Kh. Bellerby, Richard Couture, Raoul-Marie 2017 application/pdf http://hdl.handle.net/11250/2491308 https://doi.org/10.5194/gmd-10-453-2017 eng eng European Geosciences Union Norges forskningsråd: 244558 Norges forskningsråd: 254777 Norges forskningsråd: 223268 Norges forskningsråd: 208279 Norges forskningsråd: 236658 EC/FP7/265847 EC/FP7/240837 EC/H2020/654462 Geoscientific Model Development. 2017, 10 (1), 453-482. urn:issn:1991-959X http://hdl.handle.net/11250/2491308 https://doi.org/10.5194/gmd-10-453-2017 cristin:1473894 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 453-482 10 Geoscientific Model Development 1 Journal article Peer reviewed 2017 ftnorskinstvf https://doi.org/10.5194/gmd-10-453-2017 2023-02-21T08:45:07Z Interactions between seawater and benthic systems play an important role in global biogeochemical cycling. Benthic fluxes of some chemical elements (e.g., C, N, P, O, Si, Fe, Mn, S) alter the redox state and marine carbonate system (i.e., pH and carbonate saturation state), which in turn modulate the functioning of benthic and pelagic ecosystems. The redox state of the near-bottom layer in many regions can change with time, responding to the supply of organic matter, physical regime, and coastal discharge. We developed a model (BROM) to represent key biogeochemical processes in the water and sediments and to simulate changes occurring in the bottom boundary layer. BROM consists of a transport module (BROM-transport) and several biogeochemical modules that are fully compatible with the Framework for the Aquatic Biogeochemical Models, allowing independent coupling to hydrophysical models in 1-D, 2-D, or 3-D. We demonstrate that BROM is capable of simulating the seasonality in production and mineralization of organic matter as well as the mixing that leads to variations in redox conditions. BROM can be used for analyzing and interpreting data on sediment–water exchange, and for simulating the consequences of forcings such as climate change, external nutrient loading, ocean acidification, carbon storage leakage, and point-source metal pollution. publishedVersion Article in Journal/Newspaper Ocean acidification Norwegian Institute for Water research: NIVA Open Access Archive (Brage) Geoscientific Model Development 10 1 453 482 |
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Open Polar |
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Norwegian Institute for Water research: NIVA Open Access Archive (Brage) |
op_collection_id |
ftnorskinstvf |
language |
English |
description |
Interactions between seawater and benthic systems play an important role in global biogeochemical cycling. Benthic fluxes of some chemical elements (e.g., C, N, P, O, Si, Fe, Mn, S) alter the redox state and marine carbonate system (i.e., pH and carbonate saturation state), which in turn modulate the functioning of benthic and pelagic ecosystems. The redox state of the near-bottom layer in many regions can change with time, responding to the supply of organic matter, physical regime, and coastal discharge. We developed a model (BROM) to represent key biogeochemical processes in the water and sediments and to simulate changes occurring in the bottom boundary layer. BROM consists of a transport module (BROM-transport) and several biogeochemical modules that are fully compatible with the Framework for the Aquatic Biogeochemical Models, allowing independent coupling to hydrophysical models in 1-D, 2-D, or 3-D. We demonstrate that BROM is capable of simulating the seasonality in production and mineralization of organic matter as well as the mixing that leads to variations in redox conditions. BROM can be used for analyzing and interpreting data on sediment–water exchange, and for simulating the consequences of forcings such as climate change, external nutrient loading, ocean acidification, carbon storage leakage, and point-source metal pollution. publishedVersion |
format |
Article in Journal/Newspaper |
author |
Yakushev, Evgeny Protsenko, Elizaveta Bruggeman, Jorn Wallhead, Philip Pakhomova, Svetlana V. Yakubov, Shamil Kh. Bellerby, Richard Couture, Raoul-Marie |
spellingShingle |
Yakushev, Evgeny Protsenko, Elizaveta Bruggeman, Jorn Wallhead, Philip Pakhomova, Svetlana V. Yakubov, Shamil Kh. Bellerby, Richard Couture, Raoul-Marie Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
author_facet |
Yakushev, Evgeny Protsenko, Elizaveta Bruggeman, Jorn Wallhead, Philip Pakhomova, Svetlana V. Yakubov, Shamil Kh. Bellerby, Richard Couture, Raoul-Marie |
author_sort |
Yakushev, Evgeny |
title |
Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
title_short |
Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
title_full |
Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
title_fullStr |
Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
title_full_unstemmed |
Bottom RedOx Model (BROM v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
title_sort |
bottom redox model (brom v.1.1): a coupled benthic–pelagic model for simulation of water and sediment biogeochemistry |
publisher |
European Geosciences Union |
publishDate |
2017 |
url |
http://hdl.handle.net/11250/2491308 https://doi.org/10.5194/gmd-10-453-2017 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
453-482 10 Geoscientific Model Development 1 |
op_relation |
Norges forskningsråd: 244558 Norges forskningsråd: 254777 Norges forskningsråd: 223268 Norges forskningsråd: 208279 Norges forskningsråd: 236658 EC/FP7/265847 EC/FP7/240837 EC/H2020/654462 Geoscientific Model Development. 2017, 10 (1), 453-482. urn:issn:1991-959X http://hdl.handle.net/11250/2491308 https://doi.org/10.5194/gmd-10-453-2017 cristin:1473894 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/gmd-10-453-2017 |
container_title |
Geoscientific Model Development |
container_volume |
10 |
container_issue |
1 |
container_start_page |
453 |
op_container_end_page |
482 |
_version_ |
1766158499918643200 |