Physical and biological properties of early winter Antarctic sea ice in the Ross Sea

This work presents the results of physical and biological investigations at 27 biogeochemical stations of early winter sea ice in the Ross Sea during the 2017 PIPERS cruise. Only two similar cruises occurred in the past, in 1995 and 1998. The year 2017 was a specific year, in that ice growth in the...

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Main Authors: Jean-Louis Tison, Ted Maksym, Alexander D. Fraser, Matthew Corkill, Noriaki Kimura, Yuichi Nosaka, Daiki Nomura, Martin Vancoppenolle, Steve Ackley, Sharon Stammerjohn, Sarah Wauthy, Fanny Van der Linden, Gauthier Carnat, Célia Sapart, Jeroen de Jong, François Fripiat, Bruno Delille
Format: Article
Language:English
Published: Cambridge University Press 2020-12-01
Series:Annals of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0260305520000439/type/journal_article
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author Jean-Louis Tison
Ted Maksym
Alexander D. Fraser
Matthew Corkill
Noriaki Kimura
Yuichi Nosaka
Daiki Nomura
Martin Vancoppenolle
Steve Ackley
Sharon Stammerjohn
Sarah Wauthy
Fanny Van der Linden
Gauthier Carnat
Célia Sapart
Jeroen de Jong
François Fripiat
Bruno Delille
author_facet Jean-Louis Tison
Ted Maksym
Alexander D. Fraser
Matthew Corkill
Noriaki Kimura
Yuichi Nosaka
Daiki Nomura
Martin Vancoppenolle
Steve Ackley
Sharon Stammerjohn
Sarah Wauthy
Fanny Van der Linden
Gauthier Carnat
Célia Sapart
Jeroen de Jong
François Fripiat
Bruno Delille
author_sort Jean-Louis Tison
collection DOAJ
description This work presents the results of physical and biological investigations at 27 biogeochemical stations of early winter sea ice in the Ross Sea during the 2017 PIPERS cruise. Only two similar cruises occurred in the past, in 1995 and 1998. The year 2017 was a specific year, in that ice growth in the Central Ross Sea was considerably delayed, compared to previous years. These conditions resulted in lower ice thicknesses and Chl-a burdens, as compared to those observed during the previous cruises. It also resulted in a different structure of the sympagic algal community, unusually dominated by Phaeocystis rather than diatoms. Compared to autumn-winter sea ice in the Weddell Sea (AWECS cruise), the 2017 Ross Sea pack ice displayed similar thickness distribution, but much lower snow cover and therefore nearly no flooding conditions. It is shown that contrasted dynamics of autumnal-winter sea-ice growth between the Weddell Sea and the Ross Sea impacted the development of the sympagic community. Mean/median ice Chl-a concentrations were 3–5 times lower at PIPERS, and the community status there appeared to be more mature (decaying?), based on Phaeopigments/Chl-a ratios. These contrasts are discussed in the light of temporal and spatial differences between the two cruises.
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spelling doaj.art-cbc1b19c051f4970a56cc38218b5e2c52023-03-09T12:27:41ZengCambridge University PressAnnals of Glaciology0260-30551727-56442020-12-016124125910.1017/aog.2020.43Physical and biological properties of early winter Antarctic sea ice in the Ross SeaJean-Louis Tison0https://orcid.org/0000-0002-9758-3454Ted Maksym1Alexander D. Fraser2Matthew Corkill3https://orcid.org/0000-0002-5847-3738Noriaki Kimura4Yuichi Nosaka5Daiki Nomura6Martin Vancoppenolle7Steve Ackley8Sharon Stammerjohn9Sarah Wauthy10Fanny Van der Linden11https://orcid.org/0000-0002-2869-8477Gauthier Carnat12Célia Sapart13Jeroen de Jong14François Fripiat15Bruno Delille16PROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumDepartment of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, USAInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Tasmania, AustraliaInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Tasmania, Australia Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, Tasmania, AustraliaAtmosphere and Ocean Research Institute, University of Tokyo, Tokyo, JapanSchool of Biological Sciences, Tokai University, Tokyo, JapanFaculty of Fisheries Sciences, Hokkaido University, Hakodate, Japan Arctic Research Center, Hokkaido University, Sapporo, Japan Global Station for Arctic Research, Global Institution for Collaborative Research and Education, Hokkaido University, Sapporo, JapanLaboratoire d'Océanographie et du Climat, Institut Pierre-Simon Laplace, Paris, FranceDepartment of Geological Sciences, University of Texas at San Antonio, San Antonio, USAInstitute of Arctic and Alpine Research, University of Colorado, Boulder, USAPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, Belgium Unité d'Océanographie Chimique, Freshwater and Oceanic sCience Unit reSearch (FOCUS), Université de Liège, Liège, BelgiumPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumPROPICE Unit, Laboratoire de Glaciologie, Université Libre de Bruxelles, Bruxelles, BelgiumUnité d'Océanographie Chimique, Freshwater and Oceanic sCience Unit reSearch (FOCUS), Université de Liège, Liège, BelgiumThis work presents the results of physical and biological investigations at 27 biogeochemical stations of early winter sea ice in the Ross Sea during the 2017 PIPERS cruise. Only two similar cruises occurred in the past, in 1995 and 1998. The year 2017 was a specific year, in that ice growth in the Central Ross Sea was considerably delayed, compared to previous years. These conditions resulted in lower ice thicknesses and Chl-a burdens, as compared to those observed during the previous cruises. It also resulted in a different structure of the sympagic algal community, unusually dominated by Phaeocystis rather than diatoms. Compared to autumn-winter sea ice in the Weddell Sea (AWECS cruise), the 2017 Ross Sea pack ice displayed similar thickness distribution, but much lower snow cover and therefore nearly no flooding conditions. It is shown that contrasted dynamics of autumnal-winter sea-ice growth between the Weddell Sea and the Ross Sea impacted the development of the sympagic community. Mean/median ice Chl-a concentrations were 3–5 times lower at PIPERS, and the community status there appeared to be more mature (decaying?), based on Phaeopigments/Chl-a ratios. These contrasts are discussed in the light of temporal and spatial differences between the two cruises.https://www.cambridge.org/core/product/identifier/S0260305520000439/type/journal_articleAntarctic glaciologybiogeochemistrysea ice
spellingShingle Jean-Louis Tison
Ted Maksym
Alexander D. Fraser
Matthew Corkill
Noriaki Kimura
Yuichi Nosaka
Daiki Nomura
Martin Vancoppenolle
Steve Ackley
Sharon Stammerjohn
Sarah Wauthy
Fanny Van der Linden
Gauthier Carnat
Célia Sapart
Jeroen de Jong
François Fripiat
Bruno Delille
Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
Annals of Glaciology
Antarctic glaciology
biogeochemistry
sea ice
title Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
title_full Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
title_fullStr Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
title_full_unstemmed Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
title_short Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
title_sort physical and biological properties of early winter antarctic sea ice in the ross sea
topic Antarctic glaciology
biogeochemistry
sea ice
url https://www.cambridge.org/core/product/identifier/S0260305520000439/type/journal_article
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