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Assessing a turbulent mixing scheme in diurnal warm layers considering Langmuir turbulence

Assessing a turbulent mixing scheme in diurnal warm layers considering Langmuir turbulence
Assessing a turbulent mixing scheme in diurnal warm layers considering Langmuir turbulence

This study investigates how Langmuir turbulence (LT) driven by Stokes drift shear affects the heated ocean surface boundary layer (OSBL) based on turbulence-resolving large-eddy simulations (LES) and assesses an analytic vertical mixing parameterization based on a simplified second-moment closure (SMC) approach. Diurnal solar heating forces OSBL shoaling to generate a diurnal warm layer (DWL) in which heat and momentum are trapped. Without LT, relatively weak turbulent mixing results in a near-surface jet that is associated with enhanced turbulent kinetic energy (TKE) produc-tion of shear-driven turbulence (ST), which approximately balances TKE dissipation rates. Conversely, LT maintains strong mixing, delaying the DWL formation and preventing the TKE dissipation enhancement by generating a less sheared jet. However, sufficiently strong heating destroys TKE to ultimately reduce mixing and to create more sheared jets, which effectively shifts the LT to an ST-dominated regime. A second-moment turbulence budget analysis suggests that 1) the near-surface OSBL responds rapidly to the surface forcing, 2) Stokes drift impacts heat and momentum budgets in pro-foundly different ways, and 3) buoyancy terms are to leading order negligible. Building on these findings and introducing a physics-based mixing length, we develop a simplified SMC model that can be solved for near-surface expressions for key turbulent variables and mixing coefficients in terms of known variables. For ST, these expressions are consistent with the Monin–Obukhov similarity theory. For LT, these expressions reveal a fundamental dependence of turbulent variables on Stokes drift shear.

Boundary layer, Diurnal effects, Langmuir circulation, Large eddy simulations, Parameterization
0022-3670
789-808
Wang, Xingchi
39f890a7-3203-41b0-83a7-dd41bb39268a
Kukulka, Tobias
04a91e0b-1f03-40a5-b854-bda6846866db
Wang, Xingchi
39f890a7-3203-41b0-83a7-dd41bb39268a
Kukulka, Tobias
04a91e0b-1f03-40a5-b854-bda6846866db

Wang, Xingchi and Kukulka, Tobias (2025) Assessing a turbulent mixing scheme in diurnal warm layers considering Langmuir turbulence. Journal of Physical Oceanography, 55 (7), 789-808. (doi:10.1175/JPO-D-24-0164.1).

Record type: Article

Abstract

This study investigates how Langmuir turbulence (LT) driven by Stokes drift shear affects the heated ocean surface boundary layer (OSBL) based on turbulence-resolving large-eddy simulations (LES) and assesses an analytic vertical mixing parameterization based on a simplified second-moment closure (SMC) approach. Diurnal solar heating forces OSBL shoaling to generate a diurnal warm layer (DWL) in which heat and momentum are trapped. Without LT, relatively weak turbulent mixing results in a near-surface jet that is associated with enhanced turbulent kinetic energy (TKE) produc-tion of shear-driven turbulence (ST), which approximately balances TKE dissipation rates. Conversely, LT maintains strong mixing, delaying the DWL formation and preventing the TKE dissipation enhancement by generating a less sheared jet. However, sufficiently strong heating destroys TKE to ultimately reduce mixing and to create more sheared jets, which effectively shifts the LT to an ST-dominated regime. A second-moment turbulence budget analysis suggests that 1) the near-surface OSBL responds rapidly to the surface forcing, 2) Stokes drift impacts heat and momentum budgets in pro-foundly different ways, and 3) buoyancy terms are to leading order negligible. Building on these findings and introducing a physics-based mixing length, we develop a simplified SMC model that can be solved for near-surface expressions for key turbulent variables and mixing coefficients in terms of known variables. For ST, these expressions are consistent with the Monin–Obukhov similarity theory. For LT, these expressions reveal a fundamental dependence of turbulent variables on Stokes drift shear.

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Accepted/In Press date: 29 May 2025
e-pub ahead of print date: 27 June 2025
Published date: 1 July 2025
Keywords: Boundary layer, Diurnal effects, Langmuir circulation, Large eddy simulations, Parameterization

Identifiers

Local EPrints ID: 504934
URI: http://eprints.soton.ac.uk/id/eprint/504934
ISSN: 0022-3670
PURE UUID: c43261b9-68c5-4efb-8769-925fe5e6dc63
ORCID for Xingchi Wang: ORCID iD orcid.org/0000-0002-0401-4915

Catalogue record

Date deposited: 22 Sep 2025 16:58
Last modified: 23 Sep 2025 02:15

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Contributors

Author: Xingchi Wang ORCID iD
Author: Tobias Kukulka

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