Articles | Volume 19, issue 1
https://doi.org/10.5194/os-19-169-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-19-169-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Observation-based estimates of volume, heat, and freshwater exchanges between the subpolar North Atlantic interior, its boundary currents, and the atmosphere
Sam C. Jones
CORRESPONDING AUTHOR
Scottish Association for Marine Science, Oban, UK
Neil J. Fraser
Scottish Association for Marine Science, Oban, UK
Stuart A. Cunningham
Scottish Association for Marine Science, Oban, UK
Alan D. Fox
Scottish Association for Marine Science, Oban, UK
Mark E. Inall
Scottish Association for Marine Science, Oban, UK
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Short summary
Warm water is transported from the tropical Atlantic towards western Europe and the Arctic. It loses heat to the atmosphere on the way, which strongly influences the climate. We construct a dataset encircling the North Atlantic basin north of 47° N. We calculate how and where heat enters and leaves the basin and how much cooling must happen in the interior. We find that cooling in the north-eastern Atlantic is a crucial step in controlling the conversion of water to higher densities.
Warm water is transported from the tropical Atlantic towards western Europe and the Arctic. It...