A direct comparison of turbulent fluxes in ocean boundary layer vertical mixing parameterizations
ID:1132 View Protection:ATTENDEE Updated Time:2025-01-04 17:04:07 Hits:729 Poster Presentation

Start Time:2025-01-15 18:35(Asia/Shanghai)

Duration:15min

Session:S39 Session 39-Ocean Boundary Layer Turbulence: Dynamics and Its Impact on the Earth System » S39-POcean Boundary Layer Turbulence: Dynamics and Its Impact on the Earth System

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Abstract
Various ocean boundary layer vertical mixing parameterizations have been developed and a comparison among them is useful in revealing the defects of parameterizations and guiding future development. Such comparison is usually done by starting one-dimensional or three-dimensional simulations with different parameterizations from the same initial condition and running the simulations with the same forcing conditions. Differences in the simulated mean fields (e.g., velocity, temperature, salinity, etc.) and turbulent fluxes are then compared. While such approach is straightforward, errors in the simulated mean fields accumulate and are entangled with errors in the simulated turbulent fluxes. Sometimes they can partially cancel with each other and may not truly reflect the parameterization deficiencies. To address this, we directly compare the simulated vertical turbulent fluxes in single column simulations with different parameterizations and that in corresponding large eddy simulations (LES), while strongly nudging the mean fields to the LES throughout the simulations. By doing so, we have a better control that the mean fields in the single column simulations are always consistent with those of the LES during our simulations. Then, the deviations of turbulent fluxes from the LES can more fairly reflect parameterization defects. In addition, it can be regarded as an estimation of the nonlocal fluxes that a parameterization may not capture. We start with idealized open ocean cases, such as pure convection and pure shear scenarios, to demonstrate the usefulness of the method. Subsequently, we apply this method in an idealized merging boundary layer scenario, where the interaction between a surface boundary layer and a bottom boundary is important. Finally, we apply it to a more realistic case with initial conditions and forcings from the Ocean Station Papa for further method testing and parameterization comparison.
 
Keywords
ocean boundary layer turbulence, mixing parameterization comparison
Speaker
Zheng Wei
Master The Hong Kong University of Science and Technology (Guangzhou)

Submission Author
Zheng Wei The Hong Kong University of Science and Technology (Guangzhou)
Qing Li The Hong Kong University of Science and Technology (Guangzhou)
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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