On the vertical phytoplankton response to an ice free Arctic Ocean
Rapidly retreating sea ice is expected to influence future phytoplankton production in the Arctic Ocean by perturbing nutrient and light fields, but poor understanding of present phytoplankton distributions and governing mechanisms make projected changes highly uncertain. Here we use a simulation th...
Published in: | Journal of Geophysical Research: Oceans |
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Language: | English |
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Online Access: | https://eprints.soton.ac.uk/385486/ https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf |
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ftsouthampton:oai:eprints.soton.ac.uk:385486 2023-07-30T03:59:48+02:00 On the vertical phytoplankton response to an ice free Arctic Ocean Lawrence, J. Popova, E. Yool, A. Srokosz, M. 2015-12 text https://eprints.soton.ac.uk/385486/ https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf en English eng https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf Lawrence, J., Popova, E., Yool, A. and Srokosz, M. (2015) On the vertical phytoplankton response to an ice free Arctic Ocean. Journal of Geophysical Research: Oceans, 120 (12), 8571-8582. (doi:10.1002/2015JC011180 <http://dx.doi.org/10.1002/2015JC011180>). Article PeerReviewed 2015 ftsouthampton https://doi.org/10.1002/2015JC011180 2023-07-09T22:03:37Z Rapidly retreating sea ice is expected to influence future phytoplankton production in the Arctic Ocean by perturbing nutrient and light fields, but poor understanding of present phytoplankton distributions and governing mechanisms make projected changes highly uncertain. Here we use a simulation that reproduces observed seasonal phytoplankton chlorophyll distributions and annual nitrate to hypothesize that surface nitrate limitation in the Arctic Ocean deepens vertical production distributions where light-dependent growth rates are lower. We extend this to interpret depth-integrated production changes projected by the simulation for an ice-free Arctic Ocean. Future spatial changes correspond to patterns of reduced surface nitrate and increased light. Surface nitrate inventory reductions in the Beaufort Gyre and Atlantic inflow waters drive colocated production distributions deeper to where light is lower, offsetting increases in light over the water column due to reduced ice cover and thickness. Modest production increases arise, 10% in a seasonally ice-free Arctic Ocean and increasing to 30% by the end of the century, occurring at depth. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Phytoplankton Sea ice University of Southampton: e-Prints Soton Arctic Arctic Ocean Journal of Geophysical Research: Oceans 120 12 8571 8582 |
institution |
Open Polar |
collection |
University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
Rapidly retreating sea ice is expected to influence future phytoplankton production in the Arctic Ocean by perturbing nutrient and light fields, but poor understanding of present phytoplankton distributions and governing mechanisms make projected changes highly uncertain. Here we use a simulation that reproduces observed seasonal phytoplankton chlorophyll distributions and annual nitrate to hypothesize that surface nitrate limitation in the Arctic Ocean deepens vertical production distributions where light-dependent growth rates are lower. We extend this to interpret depth-integrated production changes projected by the simulation for an ice-free Arctic Ocean. Future spatial changes correspond to patterns of reduced surface nitrate and increased light. Surface nitrate inventory reductions in the Beaufort Gyre and Atlantic inflow waters drive colocated production distributions deeper to where light is lower, offsetting increases in light over the water column due to reduced ice cover and thickness. Modest production increases arise, 10% in a seasonally ice-free Arctic Ocean and increasing to 30% by the end of the century, occurring at depth. |
format |
Article in Journal/Newspaper |
author |
Lawrence, J. Popova, E. Yool, A. Srokosz, M. |
spellingShingle |
Lawrence, J. Popova, E. Yool, A. Srokosz, M. On the vertical phytoplankton response to an ice free Arctic Ocean |
author_facet |
Lawrence, J. Popova, E. Yool, A. Srokosz, M. |
author_sort |
Lawrence, J. |
title |
On the vertical phytoplankton response to an ice free Arctic Ocean |
title_short |
On the vertical phytoplankton response to an ice free Arctic Ocean |
title_full |
On the vertical phytoplankton response to an ice free Arctic Ocean |
title_fullStr |
On the vertical phytoplankton response to an ice free Arctic Ocean |
title_full_unstemmed |
On the vertical phytoplankton response to an ice free Arctic Ocean |
title_sort |
on the vertical phytoplankton response to an ice free arctic ocean |
publishDate |
2015 |
url |
https://eprints.soton.ac.uk/385486/ https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Arctic Ocean Phytoplankton Sea ice |
genre_facet |
Arctic Arctic Arctic Ocean Phytoplankton Sea ice |
op_relation |
https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf Lawrence, J., Popova, E., Yool, A. and Srokosz, M. (2015) On the vertical phytoplankton response to an ice free Arctic Ocean. Journal of Geophysical Research: Oceans, 120 (12), 8571-8582. (doi:10.1002/2015JC011180 <http://dx.doi.org/10.1002/2015JC011180>). |
op_doi |
https://doi.org/10.1002/2015JC011180 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
120 |
container_issue |
12 |
container_start_page |
8571 |
op_container_end_page |
8582 |
_version_ |
1772810574949777408 |