Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution

Patmore, Ryan D., Holland, Paul R., Vreugdenhil, Catherine A., Jenkins, Adrian and Taylor, John R. (2022) Turbulence in the ice shelf–ocean boundary current and its sensitivity to model resolution. Journal of Physical Oceanography. ISSN 0022-3670 (In Press)

[img]
Preview
Text
ISOBL.pdf - Accepted Version

Download (12MB) | Preview
Official URL: https://doi.org/10.1175/jpo-d-22-0034.1

Abstract

The ice shelf-ocean boundary current has an important control on heat delivery to the base of an ice shelf. Climate and regional models that include a representation of ice shelf cavities often use a coarse grid and results have a strong dependence on resolution near the ice shelf-ocean interface. This study models the ice shelf-ocean boundary current with a non-hydrostatic z-level configuration at turbulence-permitting resolution (1 m). The z-level model performs well when compared against state-of-the-art Large Eddy Simulations showing its capability in representing the correct physics. We showthat theoretical results from a one-dimensional model with parameterised turbulence reproduce the z-level model results to a good degree, indicating possible utility as a turbulence closure. The one-dimensional model evolves to a state of marginal instability and we use the z-level model to demonstrate how this is represented in three-dimensions. Instabilities emerge that regulate the strength of the pycnocline and coexist with persistent Ekman rolls, which are identified prior to the flow becoming intermittently unstable. When resolution of the z-level model is degraded to understand the grid-scale dependencies, the degradation is dominated by the established problem of excessive numerical diffusion. We show that at intermediate resolutions (2-4 m), the boundary layer structure can be partially recovered by tuning diffusivities. Lastly, we compare replacing prescribed melting with interactive melting that is dependent on the local ocean conditions. Interactive melting results in a feedback such that the system evolves more slowly, which is exaggerated at lower resolution.

Item Type: Article
Additional Information: Funding information: This research was funded by NERC Standard Grant NE/N010027/1.
Subjects: F700 Ocean Sciences
Department: Faculties > Engineering and Environment > Geography and Environmental Sciences
Depositing User: John Coen
Date Deposited: 16 Dec 2022 08:59
Last Modified: 16 Dec 2022 09:00
URI: https://nrl.northumbria.ac.uk/id/eprint/50905

Actions (login required)

View Item View Item

Downloads

Downloads per month over past year

View more statistics