Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean

<qd> Brown, Z. W., and Arrigo, K. R. 2012. Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean. – ICES Journal of Marine Science, 69: . </qd>Satellite remote sensing data were used to examine recent trends in sea-ice cover and net primary productivity...

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Published in:ICES Journal of Marine Science
Main Authors: Brown, Zachary W., Arrigo, Kevin R.
Format: Text
Language:English
Published: Oxford University Press 2012
Subjects:
Online Access:http://icesjms.oxfordjournals.org/cgi/content/short/69/7/1180
https://doi.org/10.1093/icesjms/fss113
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spelling fthighwire:oai:open-archive.highwire.org:icesjms:69/7/1180 2023-05-15T14:35:07+02:00 Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean Brown, Zachary W. Arrigo, Kevin R. 2012-09-01 00:00:00.0 text/html http://icesjms.oxfordjournals.org/cgi/content/short/69/7/1180 https://doi.org/10.1093/icesjms/fss113 en eng Oxford University Press http://icesjms.oxfordjournals.org/cgi/content/short/69/7/1180 http://dx.doi.org/10.1093/icesjms/fss113 Copyright (C) 2012, International Council for the Exploration of the Sea/Conseil International pour l'Exploration de la Mer Articles TEXT 2012 fthighwire https://doi.org/10.1093/icesjms/fss113 2012-08-24T19:57:06Z <qd> Brown, Z. W., and Arrigo, K. R. 2012. Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean. – ICES Journal of Marine Science, 69: . </qd>Satellite remote sensing data were used to examine recent trends in sea-ice cover and net primary productivity (NPP) in the Bering Sea and Arctic Ocean. In nearly all regions, diminished sea-ice cover significantly enhanced annual NPP, indicating that light-limitation predominates across the seasonally ice-covered waters of the northern hemisphere. However, long-term trends have not been uniform spatially. The seasonal ice pack of the Bering Sea has remained consistent over time, partially because of winter winds that have continued to carry frigid Arctic air southwards over the past six decades. Hence, apart from the “Arctic-like” Chirikov Basin (where sea-ice loss has driven a 30% increase in NPP), no secular trends are evident in Bering Sea NPP, which averaged 288 ± 26 Tg C year−1 over the satellite ocean colour record (1998–2009). Conversely, sea-ice cover in the Arctic Ocean has plummeted, extending the open-water growing season by 45 d in just 12 years, and promoting a 20% increase in NPP (range 441–585 Tg C year−1). Future sea-ice loss will likely stimulate additional NPP over the productive Bering Sea shelves, potentially reducing nutrient flux to the downstream western Arctic Ocean. Text Arctic Arctic Ocean Bering Sea ice pack Sea ice ice covered waters HighWire Press (Stanford University) Arctic Arctic Ocean Bering Sea ICES Journal of Marine Science 69 7 1180 1193
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Brown, Zachary W.
Arrigo, Kevin R.
Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
topic_facet Articles
description <qd> Brown, Z. W., and Arrigo, K. R. 2012. Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean. – ICES Journal of Marine Science, 69: . </qd>Satellite remote sensing data were used to examine recent trends in sea-ice cover and net primary productivity (NPP) in the Bering Sea and Arctic Ocean. In nearly all regions, diminished sea-ice cover significantly enhanced annual NPP, indicating that light-limitation predominates across the seasonally ice-covered waters of the northern hemisphere. However, long-term trends have not been uniform spatially. The seasonal ice pack of the Bering Sea has remained consistent over time, partially because of winter winds that have continued to carry frigid Arctic air southwards over the past six decades. Hence, apart from the “Arctic-like” Chirikov Basin (where sea-ice loss has driven a 30% increase in NPP), no secular trends are evident in Bering Sea NPP, which averaged 288 ± 26 Tg C year−1 over the satellite ocean colour record (1998–2009). Conversely, sea-ice cover in the Arctic Ocean has plummeted, extending the open-water growing season by 45 d in just 12 years, and promoting a 20% increase in NPP (range 441–585 Tg C year−1). Future sea-ice loss will likely stimulate additional NPP over the productive Bering Sea shelves, potentially reducing nutrient flux to the downstream western Arctic Ocean.
format Text
author Brown, Zachary W.
Arrigo, Kevin R.
author_facet Brown, Zachary W.
Arrigo, Kevin R.
author_sort Brown, Zachary W.
title Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
title_short Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
title_full Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
title_fullStr Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
title_full_unstemmed Contrasting trends in sea ice and primary production in the Bering Sea and Arctic Ocean
title_sort contrasting trends in sea ice and primary production in the bering sea and arctic ocean
publisher Oxford University Press
publishDate 2012
url http://icesjms.oxfordjournals.org/cgi/content/short/69/7/1180
https://doi.org/10.1093/icesjms/fss113
geographic Arctic
Arctic Ocean
Bering Sea
geographic_facet Arctic
Arctic Ocean
Bering Sea
genre Arctic
Arctic Ocean
Bering Sea
ice pack
Sea ice
ice covered waters
genre_facet Arctic
Arctic Ocean
Bering Sea
ice pack
Sea ice
ice covered waters
op_relation http://icesjms.oxfordjournals.org/cgi/content/short/69/7/1180
http://dx.doi.org/10.1093/icesjms/fss113
op_rights Copyright (C) 2012, International Council for the Exploration of the Sea/Conseil International pour l'Exploration de la Mer
op_doi https://doi.org/10.1093/icesjms/fss113
container_title ICES Journal of Marine Science
container_volume 69
container_issue 7
container_start_page 1180
op_container_end_page 1193
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