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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Bibliographic Details
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:
GE Environmental Sciences
DAS
SDG 14 - Life Below Water
GE
Antarctic
Southern Ocean
Austral
Antarc*
Sea ice
Online Access:http://hdl.handle.net/10023/28692
https://doi.org/10.1029/2023gl105139
Description
Summary: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

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