Changes between Version 2 and Version 3 of 2020WP/PHYPRO-01_agn_OSMOSIS_science
- Timestamp:
- 2020-06-02T15:54:52+02:00 (5 years ago)
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2020WP/PHYPRO-01_agn_OSMOSIS_science
v2 v3 22 22 === Description 23 23 24 Improve OSMOSIS ocean boundary layer (OBL) model in 3 areas: 24 25 26 1. Ensure consistent behaviour of OSMOSIS-OBL under ice. Revert to classic shear turbulence based on ice-ocean turbulent friction velocity where ice areal coverage is high; scale with ice fraction between shear turbulence and Langmuir turbulence model. Where Stokes drift unavailable, move to parametrised form. 27 28 2. Improve representation of OSMOSIS-OBL mixing in equatorial regions. Include mixing associated with shear of mean flow as in equatorial undercurrent. 29 30 3. Mixing in shelf seas. The OSMOSIS-OBL is primarily a surface boundary layer model and so is not set up for bottom-driven tidal mixing. We intend to transition to GLS in shelf seas. 31 32 33 34 35 36 37 25 38 26 39 === Implementation