Primary Production in Antarctic Sea Ice

A numerical model shows that in Antarctic sea ice, increased flooding in regions with thick snow cover enhances primary production in the infiltration (surface) layer. Productivity in the freeboard (sea level) layer is also determined by sea ice porosity, which varies with temperature. Spatial and t...

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Published in:Science
Main Authors: Arrigo, Kevin R., Worthen, Denise L., Lizotte, Michael P., Dixon, Paul, Dieckmann, Gerhard
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1997
Subjects:
Online Access:http://dx.doi.org/10.1126/science.276.5311.394
https://www.science.org/doi/pdf/10.1126/science.276.5311.394
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spelling craaas:10.1126/science.276.5311.394 2024-09-15T17:40:16+00:00 Primary Production in Antarctic Sea Ice Arrigo, Kevin R. Worthen, Denise L. Lizotte, Michael P. Dixon, Paul Dieckmann, Gerhard 1997 http://dx.doi.org/10.1126/science.276.5311.394 https://www.science.org/doi/pdf/10.1126/science.276.5311.394 en eng American Association for the Advancement of Science (AAAS) Science volume 276, issue 5311, page 394-397 ISSN 0036-8075 1095-9203 journal-article 1997 craaas https://doi.org/10.1126/science.276.5311.394 2024-09-05T04:01:16Z A numerical model shows that in Antarctic sea ice, increased flooding in regions with thick snow cover enhances primary production in the infiltration (surface) layer. Productivity in the freeboard (sea level) layer is also determined by sea ice porosity, which varies with temperature. Spatial and temporal variation in snow thickness and the proportion of first-year ice thus determine regional differences in sea ice primary production. Model results show that of the 40 teragrams of carbon produced annually in the Antarctic ice pack, 75 percent was associated with first-year ice and nearly 50 percent was produced in the Weddell Sea. Article in Journal/Newspaper Antarc* Antarctic ice pack Sea ice Weddell Sea AAAS Resource Center (American Association for the Advancement of Science) Science 276 5311 394 397
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description A numerical model shows that in Antarctic sea ice, increased flooding in regions with thick snow cover enhances primary production in the infiltration (surface) layer. Productivity in the freeboard (sea level) layer is also determined by sea ice porosity, which varies with temperature. Spatial and temporal variation in snow thickness and the proportion of first-year ice thus determine regional differences in sea ice primary production. Model results show that of the 40 teragrams of carbon produced annually in the Antarctic ice pack, 75 percent was associated with first-year ice and nearly 50 percent was produced in the Weddell Sea.
format Article in Journal/Newspaper
author Arrigo, Kevin R.
Worthen, Denise L.
Lizotte, Michael P.
Dixon, Paul
Dieckmann, Gerhard
spellingShingle Arrigo, Kevin R.
Worthen, Denise L.
Lizotte, Michael P.
Dixon, Paul
Dieckmann, Gerhard
Primary Production in Antarctic Sea Ice
author_facet Arrigo, Kevin R.
Worthen, Denise L.
Lizotte, Michael P.
Dixon, Paul
Dieckmann, Gerhard
author_sort Arrigo, Kevin R.
title Primary Production in Antarctic Sea Ice
title_short Primary Production in Antarctic Sea Ice
title_full Primary Production in Antarctic Sea Ice
title_fullStr Primary Production in Antarctic Sea Ice
title_full_unstemmed Primary Production in Antarctic Sea Ice
title_sort primary production in antarctic sea ice
publisher American Association for the Advancement of Science (AAAS)
publishDate 1997
url http://dx.doi.org/10.1126/science.276.5311.394
https://www.science.org/doi/pdf/10.1126/science.276.5311.394
genre Antarc*
Antarctic
ice pack
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctic
ice pack
Sea ice
Weddell Sea
op_source Science
volume 276, issue 5311, page 394-397
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.276.5311.394
container_title Science
container_volume 276
container_issue 5311
container_start_page 394
op_container_end_page 397
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