Articles | Volume 19, issue 7
https://doi.org/10.5194/gmd-19-2677-2026
https://doi.org/10.5194/gmd-19-2677-2026
Development and technical paper
 | 
09 Apr 2026
Development and technical paper |  | 09 Apr 2026

Revisiting the parameterization of dense water plume dynamics in geopotential coordinates in NEMO v4.2.2

Robinson Hordoir, Jarle Berntsen, Magnus Hieronymus, Per Pemberton, and Hjálmar Hátún

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Cited articles

Arneborg, L.: Turnover times for the water above sill level in Gullmar Fjord, Cont. Shelf Res., 24, 443–460, https://doi.org/10.1016/j.csr.2003.12.005, 2004. a
Beckmann, A. and Döscher, R.: A method for improved representation of dense water spreading over topography in geopotential-coordinate models, J. Phys. Oceanogr., 27, 581–591, 1997. a
Berntsen, J., Darelius, E., and Avlesen, H.: Topographic effects on buoyancy driven flows along the slope, Environ. Fluid Mech., 23, 369–388, https://doi.org/10.1007/s10652-022-09890-1, 2023. a
Berntsen, J., Hansen, B., Ø sterhus, S., Larsen, K. M. H., and Hátún, H.: Effects of a surface layer cross-flow and slope steepness on the rate of descent of dense water flows along a slope, Ocean Dynam., 74, 879–899, https://doi.org/10.1007/s10236-024-01642-7, 2024. a
Buckley, M. W. and Marshall, J.: Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review, Rev. Geophys., 54, 5–63, https://doi.org/10.1002/2015RG000493, 2016. a
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Short summary
Dense water created in high latitude regions flows at the bottom of the ocean, from one basin to the next, and contributes to the global ocean circulation. The flow between shallow and deeper basins occurs at straits such as the Faeroe Bank Channel as underwater streams of dense water. Their representation in ocean models is problematic. In the present article, we use a mathematical formulation of dense water plumes to show that the representation of these dense overflows can be improved.
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