Vertical structure and energetic constraints for a backscatter parameterization of ocean mesoscale eddies

E Yankovsky, S Bachman, KS Smith… - Journal of Advances in …, 2024 - Wiley Online Library
Mesoscale eddies modulate the stratification, mixing, tracer transport, and dissipation
pathways of oceanic flows over a wide range of spatiotemporal scales. The parameterization …

Toward Parameterizing Eddy-Mediated Transport of Warm Deep Water across the Weddell Sea Continental Slope

N Dettling, M Losch, F Pollmann… - Journal of Physical …, 2024 - journals.ametsoc.org
The transport of warm deep water (WDW) onto the Weddell Sea continental shelf is
associated with heat flux and strongly contributes to the melting of Antarctic ice shelves. The …

[HTML][HTML] Combined physical and biogeochemical assessment of mesoscale eddy parameterisations in ocean models: Eddy-induced advection at eddy-permitting …

X Ruan, D Couespel, M Lévy, J Li, J Mak, Y Wang - Ocean Modelling, 2024 - Elsevier
Ocean general circulation models at the eddy-permitting regime are known to under-resolve
the mesoscale eddy activity and associated eddy-mean interaction. Under-resolving the …

Edge-wave phase shifts versus normal-mode phase tilts in an Eady problem with a sloping boundary

J Mak, N Harnik, E Heifetz, G Kumar, EQY Ong - Physical Review Fluids, 2024 - APS
One mechanistic interpretation of baroclinic instability is that of mutual constructive
interference of Rossby edge waves. The suppression of baroclinic instability over slopes has …

[PDF][PDF] Implementation of a data-driven equation-discovery mesoscale parameterization into an ocean model

P Perezhogin, C Zhang, A Adcroft… - arXiv preprint arXiv …, 2023 - researchgate.net
Mesoscale eddies are poorly represented in climate ocean models, and therefore their
effects on the large scale circulation must be parameterized. Classical parameterizations …

[PDF][PDF] Vertical structure and energetic constraints for

E Yankovsky, S Bachman, KS Smith, L Zanna - researchgate.net
Ocean eddies evolving on horizontal lengthscales of order 10-100 km are not sufficiently 30
resolved in modern global ocean models that have horizontal resolutions of about 25-100 …