Articles | Volume 21, issue 7
https://doi.org/10.5194/bg-21-1961-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-21-1961-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
17 Apr 2024
Research article |
| 17 Apr 2024
| 17 Apr 2024
Vertical mixing alleviates autumnal oxygen deficiency in the central North Sea
Charlotte A. J. Williams
CORRESPONDING AUTHOR
National Oceanography Centre, Liverpool, L3 5DA, UK
Centre for Environment, Fisheries and Aquaculture Science, Lowestoft, NR33 0HT, UK
Jan Kaiser
Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, UK
Claire Mahaffey
Department of Earth, Ocean and Ecological Sciences, University of Liverpool, Liverpool, L69 3GP, UK
Naomi Greenwood
Centre for Environment, Fisheries and Aquaculture Science, Lowestoft, NR33 0HT, UK
Matthew Toberman
Scottish Association for Marine Science, Oban, Scotland, PA37 1QA, UK
Matthew R. Palmer
Plymouth Marine Laboratory, Plymouth, PL1 3DH, UK
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Short summary
Oxygen (O2) is a key indicator of ocean health. The risk of O2 loss in the productive coastal/continental slope regions is increasing. Autonomous underwater vehicles equipped with O2 optodes provide lots of data but have problems resolving strong vertical O2 changes. Here we show how to overcome this and calculate how much O2 is supplied to the low-O2 bottom waters via mixing. Bursts in mixing supply nearly all of the O2 to bottom waters in autumn, stopping them reaching ecologically low levels.
Oxygen (O2) is a key indicator of ocean health. The risk of O2 loss in the productive...
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