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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Published inAnnals of glaciology Vol. 61; no. 83; pp. 241 - 259
Main Authors Tison, Jean-Louis, Maksym, Ted, Fraser, Alexander D., Corkill, Matthew, Kimura, Noriaki, Nosaka, Yuichi, Nomura, Daiki, Vancoppenolle, Martin, Ackley, Steve, Stammerjohn, Sharon, Wauthy, Sarah, Van der Linden, Fanny, Carnat, Gauthier, Sapart, Célia, de Jong, Jeroen, Fripiat, François, Delille, Bruno
Format Journal Article Web Resource
LanguageEnglish
Published Cambridge, UK Cambridge University Press 01.12.2020
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Abstract 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.
AbstractList 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.
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.
Author Fraser, Alexander D.
Stammerjohn, Sharon
Carnat, Gauthier
Maksym, Ted
Nosaka, Yuichi
Ackley, Steve
de Jong, Jeroen
Van der Linden, Fanny
Fripiat, François
Kimura, Noriaki
Tison, Jean-Louis
Nomura, Daiki
Wauthy, Sarah
Delille, Bruno
Corkill, Matthew
Vancoppenolle, Martin
Sapart, Célia
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  organization: 13Unité d'Océanographie Chimique, Freshwater and Oceanic sCience Unit reSearch (FOCUS), Université de Liège, Liège, Belgium
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Issue 83
Keywords biogeochemistry
Antarctic glaciology
sea ice
Language English
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Snippet 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...
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StartPage 241
SubjectTerms Algae
Antarctic glaciology
Antarctic sea ice
Biogeochemistry
Biological properties
Cruises
Diatoms
Earth science
Earth Sciences
Earth sciences & physical geography
Flooding
Glaciers
Glaciology
Ice
Ice cover
Ice thickness
Marine microorganisms
Pack ice
Physical, chemical, mathematical & earth Sciences
Physique, chimie, mathématiques & sciences de la terre
Salinity
Sciences de la terre & géographie physique
Sciences of the Universe
Sea ice
Sea ice growth
Snow cover
Spatial variations
Thickness
Trends
Winter
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Title Physical and biological properties of early winter Antarctic sea ice in the Ross Sea
URI https://www.cambridge.org/core/product/identifier/S0260305520000439/type/journal_article
https://www.proquest.com/docview/2529700883
https://hal.science/hal-03030790
http://orbi.ulg.ac.be/handle/2268/249152
https://doaj.org/article/cbc1b19c051f4970a56cc38218b5e2c5
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