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.
Authors
- Ton S. van den Bremer (ORCID: https://orcid.org/0000-0001-6154-3357)
- Emiliano Renzi (ORCID: https://orcid.org/0000-0002-1459-5565)
- Alistair G.L. Borthwick (ORCID: https://orcid.org/0000-0001-6053-7764)
- Simone Michele (ORCID: https://orcid.org/0000-0002-4082-6929)
Institutions
- University of Rome Tor Vergata (IT)
- Northumbria University (GB)
- University of Plymouth (GB)
- Delft University of Technology (NL)
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