Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean
International audience The considerable uncertainties in the carbon budget of the Southern Ocean are largely attributed to unresolved variability, in particular at seasonal time scale and small spatial scale (~ 100 km). In this study, the variability of surface pCO 2 and DIC at seasonal and small-sp...
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Language: | English |
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2013
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Online Access: | https://hal.science/hal-00873740 https://hal.science/hal-00873740/document https://hal.science/hal-00873740/file/bgd-10-13855-2013.pdf https://doi.org/10.5194/BGD-10-13855-2013 |
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Open Polar |
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HAL Sorbonne Université |
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ftsorbonneuniv |
language |
English |
topic |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
spellingShingle |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] Resplandy, Laure Boutin, Jacqueline Merlivat, Liliane Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
topic_facet |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
description |
International audience The considerable uncertainties in the carbon budget of the Southern Ocean are largely attributed to unresolved variability, in particular at seasonal time scale and small spatial scale (~ 100 km). In this study, the variability of surface pCO 2 and DIC at seasonal and small-spatial scales is examined using a dataset of surface drifters including ~ 80 000 measurements at high spatio-temporal resolution. On spatial scales of 100 km, we find gradients ranging from 5 to 50 μ atm for pCO 2 and 2 to 30 μ mol kg -1 for DIC, with highest values in energetic and frontal regions. This result is supported by a second estimate obtained with SST satellite images and local DIC/SST relationships derived from drifters observations. We find that dynamical processes drives the variability of DIC at small spatial scale in most regions of the Southern Ocean, the cascade of large-scale gradients down to small spatial scales leading to gradients up to 15 μ mol kg -1 over 100 km. Although the role of biological activity is more localized, it enhances the variability up to 30 μ mol kg -1 over 100 km. The seasonal cycle of surface DIC is reconstructed following Mahadevan et al. (2011), using an annual climatology of DIC and a monthly climatology of mixed layer depth. This method is evaluated using drifters observations and proves to be a reasonable first-order estimate of the seasonality in the Southern Ocean, which could be used to validate models simulations. We find that small spatial scales structures are a non negligible source of variability for DIC, with amplitudes of about a third of the variations associated with the seasonality and up to 10 times the magnitude of large-scale gradients. The amplitude of small-scale variability reported here should be kept in mind when inferring temporal changes (seasonality, inter-annual variability, decadal trends) of the carbon budget from low resolution observations and models. |
author2 |
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Resplandy, Laure Boutin, Jacqueline Merlivat, Liliane |
author_facet |
Resplandy, Laure Boutin, Jacqueline Merlivat, Liliane |
author_sort |
Resplandy, Laure |
title |
Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
title_short |
Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
title_full |
Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
title_fullStr |
Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
title_full_unstemmed |
Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean |
title_sort |
observed small spatial scale and seasonal variability of the co 2 -system in the southern ocean |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00873740 https://hal.science/hal-00873740/document https://hal.science/hal-00873740/file/bgd-10-13855-2013.pdf https://doi.org/10.5194/BGD-10-13855-2013 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
ISSN: 1810-6277 EISSN: 1810-6285 Biogeosciences Discussions https://hal.science/hal-00873740 Biogeosciences Discussions, 2013, 10, pp.13855-13895. ⟨10.5194/BGD-10-13855-2013⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/BGD-10-13855-2013 hal-00873740 https://hal.science/hal-00873740 https://hal.science/hal-00873740/document https://hal.science/hal-00873740/file/bgd-10-13855-2013.pdf BIBCODE: 2013BGD.1013855R doi:10.5194/BGD-10-13855-2013 |
op_rights |
http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.5194/BGD-10-13855-2013 |
_version_ |
1799467259273412608 |
spelling |
ftsorbonneuniv:oai:HAL:hal-00873740v1 2024-05-19T07:48:53+00:00 Observed small spatial scale and seasonal variability of the CO 2 -system in the Southern Ocean Resplandy, Laure Boutin, Jacqueline Merlivat, Liliane Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2013-08 https://hal.science/hal-00873740 https://hal.science/hal-00873740/document https://hal.science/hal-00873740/file/bgd-10-13855-2013.pdf https://doi.org/10.5194/BGD-10-13855-2013 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/BGD-10-13855-2013 hal-00873740 https://hal.science/hal-00873740 https://hal.science/hal-00873740/document https://hal.science/hal-00873740/file/bgd-10-13855-2013.pdf BIBCODE: 2013BGD.1013855R doi:10.5194/BGD-10-13855-2013 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1810-6277 EISSN: 1810-6285 Biogeosciences Discussions https://hal.science/hal-00873740 Biogeosciences Discussions, 2013, 10, pp.13855-13895. ⟨10.5194/BGD-10-13855-2013⟩ [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2013 ftsorbonneuniv https://doi.org/10.5194/BGD-10-13855-2013 2024-04-25T04:16:22Z International audience The considerable uncertainties in the carbon budget of the Southern Ocean are largely attributed to unresolved variability, in particular at seasonal time scale and small spatial scale (~ 100 km). In this study, the variability of surface pCO 2 and DIC at seasonal and small-spatial scales is examined using a dataset of surface drifters including ~ 80 000 measurements at high spatio-temporal resolution. On spatial scales of 100 km, we find gradients ranging from 5 to 50 μ atm for pCO 2 and 2 to 30 μ mol kg -1 for DIC, with highest values in energetic and frontal regions. This result is supported by a second estimate obtained with SST satellite images and local DIC/SST relationships derived from drifters observations. We find that dynamical processes drives the variability of DIC at small spatial scale in most regions of the Southern Ocean, the cascade of large-scale gradients down to small spatial scales leading to gradients up to 15 μ mol kg -1 over 100 km. Although the role of biological activity is more localized, it enhances the variability up to 30 μ mol kg -1 over 100 km. The seasonal cycle of surface DIC is reconstructed following Mahadevan et al. (2011), using an annual climatology of DIC and a monthly climatology of mixed layer depth. This method is evaluated using drifters observations and proves to be a reasonable first-order estimate of the seasonality in the Southern Ocean, which could be used to validate models simulations. We find that small spatial scales structures are a non negligible source of variability for DIC, with amplitudes of about a third of the variations associated with the seasonality and up to 10 times the magnitude of large-scale gradients. The amplitude of small-scale variability reported here should be kept in mind when inferring temporal changes (seasonality, inter-annual variability, decadal trends) of the carbon budget from low resolution observations and models. Article in Journal/Newspaper Southern Ocean HAL Sorbonne Université |