Characterization of distinct bloom phenology regimes in the Southern Ocean

Abstract In this study, we document the regional variations of bloom phenology in the Southern Ocean, based on a 13-year product of ocean colour measurements co-located with observation-based estimates of the mixed-layer depth. One key aspect of our work is to discriminate between mixed-layer integr...

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Published in:ICES Journal of Marine Science
Main Authors: Sallée, Jean-Baptiste, Llort, J., Tagliabue, A., Lévy, M.
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2015
Subjects:
Online Access:http://dx.doi.org/10.1093/icesjms/fsv069
http://academic.oup.com/icesjms/article-pdf/72/6/1985/31226128/fsv069.pdf
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spelling croxfordunivpr:10.1093/icesjms/fsv069 2024-10-13T14:03:14+00:00 Characterization of distinct bloom phenology regimes in the Southern Ocean Sallée, Jean-Baptiste Llort, J. Tagliabue, A. Lévy, M. 2015 http://dx.doi.org/10.1093/icesjms/fsv069 http://academic.oup.com/icesjms/article-pdf/72/6/1985/31226128/fsv069.pdf en eng Oxford University Press (OUP) ICES Journal of Marine Science volume 72, issue 6, page 1985-1998 ISSN 1095-9289 1054-3139 journal-article 2015 croxfordunivpr https://doi.org/10.1093/icesjms/fsv069 2024-09-17T04:29:40Z Abstract In this study, we document the regional variations of bloom phenology in the Southern Ocean, based on a 13-year product of ocean colour measurements co-located with observation-based estimates of the mixed-layer depth. One key aspect of our work is to discriminate between mixed-layer integrated blooms and surface blooms. By segregating blooms that occur before or after the winter solstice and blooms where integrated and surface biomass increase together or display a lag, we define three dominating Southern Ocean bloom regimes. While the regime definitions are solely based on bloom timing characteristics, the three regimes organize coherently in geographical space, and are associated with distinct dynamical regions of the Southern Ocean: the subtropics, the subantarctic, and the Antarctic Circumpolar Current region. All regimes have their mixed-layer integrated onset between autumn and winter, when the daylength is short and the mixed layer actively mixes and deepens. We discuss how these autumn–winter bloom onsets are controlled by either nutrient entrainment and/or reduction in prey-grazer encounter rate. In addition to the autumn–winter biomass increase, the subantarctic regime has a significant spring biomass growth associated with the shutdown of turbulence when air–sea heat flux switches from surface cooling to surface warming. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Oxford University Press Antarctic Southern Ocean The Antarctic ICES Journal of Marine Science 72 6 1985 1998
institution Open Polar
collection Oxford University Press
op_collection_id croxfordunivpr
language English
description Abstract In this study, we document the regional variations of bloom phenology in the Southern Ocean, based on a 13-year product of ocean colour measurements co-located with observation-based estimates of the mixed-layer depth. One key aspect of our work is to discriminate between mixed-layer integrated blooms and surface blooms. By segregating blooms that occur before or after the winter solstice and blooms where integrated and surface biomass increase together or display a lag, we define three dominating Southern Ocean bloom regimes. While the regime definitions are solely based on bloom timing characteristics, the three regimes organize coherently in geographical space, and are associated with distinct dynamical regions of the Southern Ocean: the subtropics, the subantarctic, and the Antarctic Circumpolar Current region. All regimes have their mixed-layer integrated onset between autumn and winter, when the daylength is short and the mixed layer actively mixes and deepens. We discuss how these autumn–winter bloom onsets are controlled by either nutrient entrainment and/or reduction in prey-grazer encounter rate. In addition to the autumn–winter biomass increase, the subantarctic regime has a significant spring biomass growth associated with the shutdown of turbulence when air–sea heat flux switches from surface cooling to surface warming.
format Article in Journal/Newspaper
author Sallée, Jean-Baptiste
Llort, J.
Tagliabue, A.
Lévy, M.
spellingShingle Sallée, Jean-Baptiste
Llort, J.
Tagliabue, A.
Lévy, M.
Characterization of distinct bloom phenology regimes in the Southern Ocean
author_facet Sallée, Jean-Baptiste
Llort, J.
Tagliabue, A.
Lévy, M.
author_sort Sallée, Jean-Baptiste
title Characterization of distinct bloom phenology regimes in the Southern Ocean
title_short Characterization of distinct bloom phenology regimes in the Southern Ocean
title_full Characterization of distinct bloom phenology regimes in the Southern Ocean
title_fullStr Characterization of distinct bloom phenology regimes in the Southern Ocean
title_full_unstemmed Characterization of distinct bloom phenology regimes in the Southern Ocean
title_sort characterization of distinct bloom phenology regimes in the southern ocean
publisher Oxford University Press (OUP)
publishDate 2015
url http://dx.doi.org/10.1093/icesjms/fsv069
http://academic.oup.com/icesjms/article-pdf/72/6/1985/31226128/fsv069.pdf
geographic Antarctic
Southern Ocean
The Antarctic
geographic_facet Antarctic
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_source ICES Journal of Marine Science
volume 72, issue 6, page 1985-1998
ISSN 1095-9289 1054-3139
op_doi https://doi.org/10.1093/icesjms/fsv069
container_title ICES Journal of Marine Science
container_volume 72
container_issue 6
container_start_page 1985
op_container_end_page 1998
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