Heat transfer and mass transport in the ocean wave-driven free-surface boundary layer

We present a mathematical model to investigate heat transfer and mass transport dynamics in the wave-driven free-surface boundary layer of the ocean under the influence of long-crested progressive surface gravity waves. The continuity, momentum and convection–diffusion equations for fluid temperature are solved within a Lagrangian framework. We assume that eddy viscosity and thermometric conductivity are dependent on Lagrangian coordinates, and derive a new form of the second-order Lagrangian mass transport velocity, applicable across the entire finite water depth. We then analyse the convective heat dynamics influenced by the free-surface boundary layer. Rectangular distributions of free-surface temperature (i.e. a Dirichlet boundary condition) are considered, and analytical solutions for thermal boundary layer temperature fields are provided to offer insights into free-surface heat transfer mechanisms affected by ocean waves. Our results suggest the need to improve existing models that neglect the effects of free-surface waves and the free-surface boundary layer on ocean mass transport and heat transfer.

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Publication Details

Journal
Journal of Fluid Mechanics
Published
2025-04-25
DOI
https://doi.org/10.1017/jfm.2025.308
Citations
3
Primary Topic
Ocean Waves and Remote Sensing
Type
article
Field-Weighted Citation Impact
5.38
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article

Heat transfer and mass transport in the ocean wave-driven free-surface boundary layer

Ton S. van den Bremer, Emiliano Renzi, Alistair G.L. Borthwick, Simone Michele
3 citations
Journal of Fluid Mechanics
Ocean Waves and Remote Sensing
5.38
article

Heat transfer and mass transport in the ocean wave-driven free-surface boundary layer

Ton S. van den Bremer, Emiliano Renzi, Alistair G.L. Borthwick, Simone Michele
article en
3 citations

Abstract

We present a mathematical model to investigate heat transfer and mass transport dynamics in the wave-driven free-surface boundary layer of the ocean under the influence of long-crested progressive surface gravity waves. The continuity, momentum and convection–diffusion equations for fluid temperature are solved within a Lagrangian framework. We assume that eddy viscosity and thermometric conductivity are dependent on Lagrangian coordinates, and derive a new form of the second-order Lagrangian mass transport velocity, applicable across the entire finite water depth. We then analyse the convective heat dynamics influenced by the free-surface boundary layer. Rectangular distributions of free-surface temperature (i.e. a Dirichlet boundary condition) are considered, and analytical solutions for thermal boundary layer temperature fields are provided to offer insights into free-surface heat transfer mechanisms affected by ocean waves. Our results suggest the need to improve existing models that neglect the effects of free-surface waves and the free-surface boundary layer on ocean mass transport and heat transfer.

Journal of Fluid MechanicsVol. 1010
University of Rome Tor Vergata (IT), Northumbria University (GB), University of Plymouth (GB), Delft University of Technology (NL)
Openalex Percentile: Top 5%
Ocean Waves and Remote Sensing
5.38
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