Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)

International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in d...

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Published in:Global Biogeochemical Cycles
Main Authors: Najjar, R., Jin, X., Louanchi, F., Aumont, O., Caldeira, K., Doney, S., Dutay, J.-C., Follows, M., Gruber, N., Joos, F., Lindsay, K., Maier-Reimer, E., Matear, R., Matsumoto, K., Monfray, P., Mouchet, A., Orr, J., Plattner, G.-K., Sarmiento, J., Schlitzer, R., Slater, R., Weirig, M.-F., Yamanaka, Y., Yool, A.
Other Authors: PennState Meteorology Department, Pennsylvania State University (Penn State), Penn State System-Penn State System, Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Modélisation du climat (CLIM), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
Online Access:https://hal.science/hal-03096840
https://hal.science/hal-03096840/document
https://hal.science/hal-03096840/file/2006GB002857.pdf
https://doi.org/10.1029/2006GB002857
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record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in different coarse-resolution ocean circulation models. The model mean (±1s) downward flux of organic matter across 75 m depth is 17 ± 6 Pg C yr À1. Model means of globally averaged particle export, the fraction of total export in dissolved form, surface semilabile dissolved organic carbon (DOC), and seasonal net outgassing (SNO) of oxygen are in good agreement with observation-based estimates, but particle export and surface DOC are too high in the tropics. There is a high sensitivity of the results to circulation, as evidenced by (1) the correlation of surface DOC and export with circulation metrics, including chlorofluorocarbon inventory and deep-ocean radiocarbon, (2) very large intermodel differences in Southern Ocean export, and (3) greater export production, fraction of export as DOM, and SNO in models with explicit mixed layer physics. However, deep-ocean oxygen, which varies widely among the models, is poorly correlated with other model indices. Cross-model means of several biogeochemical metrics show better agreement with observation-based estimates when restricted to those models that best simulate deep-ocean radiocarbon. Overall, the results emphasize the importance of physical processes in marine biogeochemical modeling and suggest that the development of circulation models can be accelerated by evaluating them with marine biogeochemical metrics.
author2 PennState Meteorology Department
Pennsylvania State University (Penn State)
Penn State System-Penn State System
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Modélisation du climat (CLIM)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
format Article in Journal/Newspaper
author Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
author_facet Najjar, R.
Jin, X.
Louanchi, F.
Aumont, O.
Caldeira, K.
Doney, S.
Dutay, J.-C.
Follows, M.
Gruber, N.
Joos, F.
Lindsay, K.
Maier-Reimer, E.
Matear, R.
Matsumoto, K.
Monfray, P.
Mouchet, A.
Orr, J.
Plattner, G.-K.
Sarmiento, J.
Schlitzer, R.
Slater, R.
Weirig, M.-F.
Yamanaka, Y.
Yool, A.
author_sort Najjar, R.
title Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_short Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_full Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_fullStr Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_full_unstemmed Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2)
title_sort impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: results from phase ii of the ocean carbon-cycle model intercomparison project (ocmip-2)
publisher HAL CCSD
publishDate 2007
url https://hal.science/hal-03096840
https://hal.science/hal-03096840/document
https://hal.science/hal-03096840/file/2006GB002857.pdf
https://doi.org/10.1029/2006GB002857
genre Southern Ocean
genre_facet Southern Ocean
op_source ISSN: 0886-6236
EISSN: 1944-8224
Global Biogeochemical Cycles
https://hal.science/hal-03096840
Global Biogeochemical Cycles, 2007, 21 (3), pp.n/a-n/a. ⟨10.1029/2006GB002857⟩
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doi:10.1029/2006GB002857
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2006GB002857
container_title Global Biogeochemical Cycles
container_volume 21
container_issue 3
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spelling ftinsu:oai:HAL:hal-03096840v1 2024-04-28T08:39:39+00:00 Impact of circulation on export production, dissolved organic matter, and dissolved oxygen in the ocean: Results from Phase II of the Ocean Carbon-cycle Model Intercomparison Project (OCMIP-2) Najjar, R. Jin, X. Louanchi, F. Aumont, O. Caldeira, K. Doney, S. Dutay, J.-C. Follows, M. Gruber, N. Joos, F. Lindsay, K. Maier-Reimer, E. Matear, R. Matsumoto, K. Monfray, P. Mouchet, A. Orr, J. Plattner, G.-K. Sarmiento, J. Schlitzer, R. Slater, R. Weirig, M.-F. Yamanaka, Y. Yool, A. PennState Meteorology Department Pennsylvania State University (Penn State) Penn State System-Penn State System Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Modélisation du climat (CLIM) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) 2007-09 https://hal.science/hal-03096840 https://hal.science/hal-03096840/document https://hal.science/hal-03096840/file/2006GB002857.pdf https://doi.org/10.1029/2006GB002857 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2006GB002857 hal-03096840 https://hal.science/hal-03096840 https://hal.science/hal-03096840/document https://hal.science/hal-03096840/file/2006GB002857.pdf doi:10.1029/2006GB002857 info:eu-repo/semantics/OpenAccess ISSN: 0886-6236 EISSN: 1944-8224 Global Biogeochemical Cycles https://hal.science/hal-03096840 Global Biogeochemical Cycles, 2007, 21 (3), pp.n/a-n/a. ⟨10.1029/2006GB002857⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2007 ftinsu https://doi.org/10.1029/2006GB002857 2024-04-05T00:39:09Z International audience Results are presented of export production, dissolved organic matter (DOM) and dissolved oxygen simulated by 12 global ocean models participating in the second phase of the Ocean Carbon-cycle Model Intercomparison Project. A common, simple biogeochemical model is utilized in different coarse-resolution ocean circulation models. The model mean (±1s) downward flux of organic matter across 75 m depth is 17 ± 6 Pg C yr À1. Model means of globally averaged particle export, the fraction of total export in dissolved form, surface semilabile dissolved organic carbon (DOC), and seasonal net outgassing (SNO) of oxygen are in good agreement with observation-based estimates, but particle export and surface DOC are too high in the tropics. There is a high sensitivity of the results to circulation, as evidenced by (1) the correlation of surface DOC and export with circulation metrics, including chlorofluorocarbon inventory and deep-ocean radiocarbon, (2) very large intermodel differences in Southern Ocean export, and (3) greater export production, fraction of export as DOM, and SNO in models with explicit mixed layer physics. However, deep-ocean oxygen, which varies widely among the models, is poorly correlated with other model indices. Cross-model means of several biogeochemical metrics show better agreement with observation-based estimates when restricted to those models that best simulate deep-ocean radiocarbon. Overall, the results emphasize the importance of physical processes in marine biogeochemical modeling and suggest that the development of circulation models can be accelerated by evaluating them with marine biogeochemical metrics. Article in Journal/Newspaper Southern Ocean Institut national des sciences de l'Univers: HAL-INSU Global Biogeochemical Cycles 21 3 n/a n/a