Role of sea ice in global biogeochemical cycles: emerging views and challenges
International audience Observations from the last decade suggest an important role of sea ice in the global biogeochemical cycles, promoted by (i) active biological and chemical processes within the sea ice; (ii) fluid and gas exchanges at the sea ice interface through an often permeable sea ice cov...
Published in: | Quaternary Science Reviews |
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Main Authors: | , , , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2013
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Subjects: | |
Online Access: | https://hal.science/hal-00912608 https://hal.science/hal-00912608/document https://hal.science/hal-00912608/file/Vancoppenolle_et_al_QSR13_revised.pdf https://doi.org/10.1016/J.QUASCIREV.2013.04.011 |
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ftepunivpsaclay:oai:HAL:hal-00912608v1 |
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openpolar |
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Open Polar |
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École Polytechnique, Université Paris-Saclay: HAL |
op_collection_id |
ftepunivpsaclay |
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] Vancoppenolle, Martin Meiners, Klaus M. Michel, Christine Bopp, Laurent Brabant, Frédéric Carnat, Gauthier Delille, Bruno Lannuzel, Delphine Madec, Gurvan Moreau, Sébastien Tison, Jean-Louis van Der Merwe, Pier Role of sea ice in global biogeochemical cycles: emerging views and challenges |
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 Observations from the last decade suggest an important role of sea ice in the global biogeochemical cycles, promoted by (i) active biological and chemical processes within the sea ice; (ii) fluid and gas exchanges at the sea ice interface through an often permeable sea ice cover; and (iii) tight physical, biological and chemical interactions between the sea ice, the ocean and the atmosphere. Photosynthetic micro-organisms in sea ice thrive in liquid brine inclusions encased in a pure ice matrix, where they find suitable light and nutrient levels. They extend the production season, provide a winter and early spring food source, and contribute to organic carbon export to depth. Under-ice and ice edge phytoplankton blooms occur when ice retreats, favoured by increasing light, stratification, and by the release of material into the water column. In particular, the release of iron - highly concentrated in sea ice - could have large effects in the iron-limited Southern Ocean. The export of inorganic carbon transport by brine sinking below the mixed layer, calcium carbonate precipitation in sea ice, as well as active ice-atmosphere carbon dioxide (CO 2 ) fluxes, could play a central role in the marine carbon cycle. Sea ice processes could also significantly contribute to the sulphur cycle through the large production by ice algae of dimethylsulfoniopropionate (DMSP), the precursor of sulphate aerosols, which as cloud condensation nuclei have a potential cooling effect on the planet. Finally, the sea ice zone supports significant ocean-atmosphere methane (CH 4 ) fluxes, while saline ice surfaces activate springtime atmospheric bromine chemistry, setting ground for tropospheric ozone depletion events observed near both poles. All these mechanisms are generally known, but neither precisely understood nor quantified at large scales. As polar regions are rapidly changing, understanding the large-scale polar marine biogeochemical processes and their future evolution is of high priority. Earth system ... |
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) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Australian Antarctic Division (AAD) Australian Government, Department of the Environment and Energy Fisheries & Oceans Canada 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) Laboratoire de Glaciologie Bruxelles Université libre de Bruxelles (ULB) Unité d'Océanographie Chimique Interfacultary Center for Marine Research (MARE) Université de Liège-Université de Liège National Oceanography Centre Southampton (NOC) University of Southampton Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM) Earth and Life Institute Louvain-La-Neuve (ELI) Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL) |
format |
Article in Journal/Newspaper |
author |
Vancoppenolle, Martin Meiners, Klaus M. Michel, Christine Bopp, Laurent Brabant, Frédéric Carnat, Gauthier Delille, Bruno Lannuzel, Delphine Madec, Gurvan Moreau, Sébastien Tison, Jean-Louis van Der Merwe, Pier |
author_facet |
Vancoppenolle, Martin Meiners, Klaus M. Michel, Christine Bopp, Laurent Brabant, Frédéric Carnat, Gauthier Delille, Bruno Lannuzel, Delphine Madec, Gurvan Moreau, Sébastien Tison, Jean-Louis van Der Merwe, Pier |
author_sort |
Vancoppenolle, Martin |
title |
Role of sea ice in global biogeochemical cycles: emerging views and challenges |
title_short |
Role of sea ice in global biogeochemical cycles: emerging views and challenges |
title_full |
Role of sea ice in global biogeochemical cycles: emerging views and challenges |
title_fullStr |
Role of sea ice in global biogeochemical cycles: emerging views and challenges |
title_full_unstemmed |
Role of sea ice in global biogeochemical cycles: emerging views and challenges |
title_sort |
role of sea ice in global biogeochemical cycles: emerging views and challenges |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal.science/hal-00912608 https://hal.science/hal-00912608/document https://hal.science/hal-00912608/file/Vancoppenolle_et_al_QSR13_revised.pdf https://doi.org/10.1016/J.QUASCIREV.2013.04.011 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
ice algae Sea ice Southern Ocean |
genre_facet |
ice algae Sea ice Southern Ocean |
op_source |
ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-00912608 Quaternary Science Reviews, 2013, 79, pp.207-230. ⟨10.1016/J.QUASCIREV.2013.04.011⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/J.QUASCIREV.2013.04.011 hal-00912608 https://hal.science/hal-00912608 https://hal.science/hal-00912608/document https://hal.science/hal-00912608/file/Vancoppenolle_et_al_QSR13_revised.pdf BIBCODE: 2013QSRv.79.207V doi:10.1016/J.QUASCIREV.2013.04.011 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/J.QUASCIREV.2013.04.011 |
container_title |
Quaternary Science Reviews |
container_volume |
79 |
container_start_page |
207 |
op_container_end_page |
230 |
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1801376583348387840 |
spelling |
ftepunivpsaclay:oai:HAL:hal-00912608v1 2024-06-09T07:46:37+00:00 Role of sea ice in global biogeochemical cycles: emerging views and challenges Vancoppenolle, Martin Meiners, Klaus M. Michel, Christine Bopp, Laurent Brabant, Frédéric Carnat, Gauthier Delille, Bruno Lannuzel, Delphine Madec, Gurvan Moreau, Sébastien Tison, Jean-Louis van Der Merwe, Pier 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) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Australian Antarctic Division (AAD) Australian Government, Department of the Environment and Energy Fisheries & Oceans Canada 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) Laboratoire de Glaciologie Bruxelles Université libre de Bruxelles (ULB) Unité d'Océanographie Chimique Interfacultary Center for Marine Research (MARE) Université de Liège-Université de Liège National Oceanography Centre Southampton (NOC) University of Southampton Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM) Earth and Life Institute Louvain-La-Neuve (ELI) Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL) 2013-11 https://hal.science/hal-00912608 https://hal.science/hal-00912608/document https://hal.science/hal-00912608/file/Vancoppenolle_et_al_QSR13_revised.pdf https://doi.org/10.1016/J.QUASCIREV.2013.04.011 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/J.QUASCIREV.2013.04.011 hal-00912608 https://hal.science/hal-00912608 https://hal.science/hal-00912608/document https://hal.science/hal-00912608/file/Vancoppenolle_et_al_QSR13_revised.pdf BIBCODE: 2013QSRv.79.207V doi:10.1016/J.QUASCIREV.2013.04.011 info:eu-repo/semantics/OpenAccess ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-00912608 Quaternary Science Reviews, 2013, 79, pp.207-230. ⟨10.1016/J.QUASCIREV.2013.04.011⟩ [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 ftepunivpsaclay https://doi.org/10.1016/J.QUASCIREV.2013.04.011 2024-05-16T12:10:49Z International audience Observations from the last decade suggest an important role of sea ice in the global biogeochemical cycles, promoted by (i) active biological and chemical processes within the sea ice; (ii) fluid and gas exchanges at the sea ice interface through an often permeable sea ice cover; and (iii) tight physical, biological and chemical interactions between the sea ice, the ocean and the atmosphere. Photosynthetic micro-organisms in sea ice thrive in liquid brine inclusions encased in a pure ice matrix, where they find suitable light and nutrient levels. They extend the production season, provide a winter and early spring food source, and contribute to organic carbon export to depth. Under-ice and ice edge phytoplankton blooms occur when ice retreats, favoured by increasing light, stratification, and by the release of material into the water column. In particular, the release of iron - highly concentrated in sea ice - could have large effects in the iron-limited Southern Ocean. The export of inorganic carbon transport by brine sinking below the mixed layer, calcium carbonate precipitation in sea ice, as well as active ice-atmosphere carbon dioxide (CO 2 ) fluxes, could play a central role in the marine carbon cycle. Sea ice processes could also significantly contribute to the sulphur cycle through the large production by ice algae of dimethylsulfoniopropionate (DMSP), the precursor of sulphate aerosols, which as cloud condensation nuclei have a potential cooling effect on the planet. Finally, the sea ice zone supports significant ocean-atmosphere methane (CH 4 ) fluxes, while saline ice surfaces activate springtime atmospheric bromine chemistry, setting ground for tropospheric ozone depletion events observed near both poles. All these mechanisms are generally known, but neither precisely understood nor quantified at large scales. As polar regions are rapidly changing, understanding the large-scale polar marine biogeochemical processes and their future evolution is of high priority. Earth system ... Article in Journal/Newspaper ice algae Sea ice Southern Ocean École Polytechnique, Université Paris-Saclay: HAL Southern Ocean Quaternary Science Reviews 79 207 230 |