Potential predictability of the spring bloom in the Southern Ocean sea ice zone

This work was supported by the High Meadows Environmental Institute at Princeton University and the NSF's Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) Project under the NSF Award PLR-1425989. F.A.H. was supported by NASA Grant 80NSSC19K1115 and by the European Union (ERC...

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Published in:Geophysical Research Letters
Main Authors: Buchovecky, Benjamin, MacGilchrist, Graeme A., Bushuk, Mitchell, Haumann, F. Alexander, Frölicher, Thomas L., Le Grix, Natacha, Dunne, John
Other Authors: University of St Andrews. School of Earth & Environmental Sciences
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
DAS
GE
Online Access:http://hdl.handle.net/10023/28692
https://doi.org/10.1029/2023gl105139
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spelling ftstandrewserep:oai:research-repository.st-andrews.ac.uk:10023/28692 2023-12-17T10:20:37+01:00 Potential predictability of the spring bloom in the Southern Ocean sea ice zone Buchovecky, Benjamin MacGilchrist, Graeme A. Bushuk, Mitchell Haumann, F. Alexander Frölicher, Thomas L. Le Grix, Natacha Dunne, John University of St Andrews. School of Earth & Environmental Sciences 2023-11-14T11:30:06Z application/pdf http://hdl.handle.net/10023/28692 https://doi.org/10.1029/2023gl105139 eng eng Geophysical Research Letters Buchovecky , B , MacGilchrist , G A , Bushuk , M , Haumann , F A , Frölicher , T L , Le Grix , N & Dunne , J 2023 , ' Potential predictability of the spring bloom in the Southern Ocean sea ice zone ' , Geophysical Research Letters , vol. 50 , no. 20 , e2023GL105139 . https://doi.org/10.1029/2023gl105139 0094-8276 PURE: 296374514 PURE UUID: 2cb54d7e-e0e3-4786-9371-bca795be357a Jisc: 1416618 Scopus: 85174446236 ORCID: /0000-0003-1409-8937/work/146964133 http://hdl.handle.net/10023/28692 https://doi.org/10.1029/2023gl105139 Copyright © 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited. GE Environmental Sciences DAS SDG 14 - Life Below Water GE Journal article 2023 ftstandrewserep https://doi.org/10.1029/2023gl105139 2023-11-23T23:29:14Z This work was supported by the High Meadows Environmental Institute at Princeton University and the NSF's Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) Project under the NSF Award PLR-1425989. F.A.H. was supported by NASA Grant 80NSSC19K1115 and by the European Union (ERC, VERTEXSO, 101041743). G.A.M was supported under SOCCOM and UKRI Grant MR/W013835/1. T.L.F was supported by Swiss National Science Foundation (Grant P00P2_198897) and the Swiss National Supercomputing Centre. N.L was supported by the European Union's Horizon 2020 research and innovation program under Grant 820989 (project COMFORT) and no. 862923 (project AtlantECO) as well as the Bretscher Funds. Every austral spring when Antarctic sea ice melts, favorable growing conditions lead to an intense phytoplankton bloom, which supports much of the local marine ecosystem. Recent studies have found that Antarctic sea ice is predictable several years in advance, suggesting that the spring bloom might exhibit similar predictability. Using a suite of perfect model predictability experiments, we find that November net primary production (NPP) is potentially predictable 7 to 10 years in advance in many Southern Ocean regions. Sea ice extent predictability peaks in late winter, followed by absorbed shortwave radiation and NPP with a 2 to 3 months lag. This seasonal progression of predictability supports our hypothesis that sea ice and light limitation control the inherent predictability of the spring bloom. Our results suggest skillful interannual predictions of NPP may be achievable, with implications for managing fisheries and the marine ecosystem, and guiding conservation policy in the Southern Ocean. Publisher PDF Peer reviewed Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean University of St Andrews: Digital Research Repository Antarctic Southern Ocean Austral Geophysical Research Letters 50 20
institution Open Polar
collection University of St Andrews: Digital Research Repository
op_collection_id ftstandrewserep
language English
topic GE Environmental Sciences
DAS
SDG 14 - Life Below Water
GE
spellingShingle GE Environmental Sciences
DAS
SDG 14 - Life Below Water
GE
Buchovecky, Benjamin
MacGilchrist, Graeme A.
Bushuk, Mitchell
Haumann, F. Alexander
Frölicher, Thomas L.
Le Grix, Natacha
Dunne, John
Potential predictability of the spring bloom in the Southern Ocean sea ice zone
topic_facet GE Environmental Sciences
DAS
SDG 14 - Life Below Water
GE
description This work was supported by the High Meadows Environmental Institute at Princeton University and the NSF's Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) Project under the NSF Award PLR-1425989. F.A.H. was supported by NASA Grant 80NSSC19K1115 and by the European Union (ERC, VERTEXSO, 101041743). G.A.M was supported under SOCCOM and UKRI Grant MR/W013835/1. T.L.F was supported by Swiss National Science Foundation (Grant P00P2_198897) and the Swiss National Supercomputing Centre. N.L was supported by the European Union's Horizon 2020 research and innovation program under Grant 820989 (project COMFORT) and no. 862923 (project AtlantECO) as well as the Bretscher Funds. Every austral spring when Antarctic sea ice melts, favorable growing conditions lead to an intense phytoplankton bloom, which supports much of the local marine ecosystem. Recent studies have found that Antarctic sea ice is predictable several years in advance, suggesting that the spring bloom might exhibit similar predictability. Using a suite of perfect model predictability experiments, we find that November net primary production (NPP) is potentially predictable 7 to 10 years in advance in many Southern Ocean regions. Sea ice extent predictability peaks in late winter, followed by absorbed shortwave radiation and NPP with a 2 to 3 months lag. This seasonal progression of predictability supports our hypothesis that sea ice and light limitation control the inherent predictability of the spring bloom. Our results suggest skillful interannual predictions of NPP may be achievable, with implications for managing fisheries and the marine ecosystem, and guiding conservation policy in the Southern Ocean. Publisher PDF Peer reviewed
author2 University of St Andrews. School of Earth & Environmental Sciences
format Article in Journal/Newspaper
author Buchovecky, Benjamin
MacGilchrist, Graeme A.
Bushuk, Mitchell
Haumann, F. Alexander
Frölicher, Thomas L.
Le Grix, Natacha
Dunne, John
author_facet Buchovecky, Benjamin
MacGilchrist, Graeme A.
Bushuk, Mitchell
Haumann, F. Alexander
Frölicher, Thomas L.
Le Grix, Natacha
Dunne, John
author_sort Buchovecky, Benjamin
title Potential predictability of the spring bloom in the Southern Ocean sea ice zone
title_short Potential predictability of the spring bloom in the Southern Ocean sea ice zone
title_full Potential predictability of the spring bloom in the Southern Ocean sea ice zone
title_fullStr Potential predictability of the spring bloom in the Southern Ocean sea ice zone
title_full_unstemmed Potential predictability of the spring bloom in the Southern Ocean sea ice zone
title_sort potential predictability of the spring bloom in the southern ocean sea ice zone
publishDate 2023
url http://hdl.handle.net/10023/28692
https://doi.org/10.1029/2023gl105139
geographic Antarctic
Southern Ocean
Austral
geographic_facet Antarctic
Southern Ocean
Austral
genre Antarc*
Antarctic
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Sea ice
Southern Ocean
op_relation Geophysical Research Letters
Buchovecky , B , MacGilchrist , G A , Bushuk , M , Haumann , F A , Frölicher , T L , Le Grix , N & Dunne , J 2023 , ' Potential predictability of the spring bloom in the Southern Ocean sea ice zone ' , Geophysical Research Letters , vol. 50 , no. 20 , e2023GL105139 . https://doi.org/10.1029/2023gl105139
0094-8276
PURE: 296374514
PURE UUID: 2cb54d7e-e0e3-4786-9371-bca795be357a
Jisc: 1416618
Scopus: 85174446236
ORCID: /0000-0003-1409-8937/work/146964133
http://hdl.handle.net/10023/28692
https://doi.org/10.1029/2023gl105139
op_rights Copyright © 2023. The Authors. This is an open access article under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
op_doi https://doi.org/10.1029/2023gl105139
container_title Geophysical Research Letters
container_volume 50
container_issue 20
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