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...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Lawrence, J., Popova, E., Yool, A., Srokosz, M.
Format: Article in Journal/Newspaper
Language:English
Published: 2015
Subjects:
Online Access:https://eprints.soton.ac.uk/385486/
https://eprints.soton.ac.uk/385486/1/jgrc21532.pdf
id ftsouthampton:oai:eprints.soton.ac.uk:385486
record_format openpolar
spelling 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