Articles | Volume 21, issue 5
https://doi.org/10.5194/os-21-1943-2025
https://doi.org/10.5194/os-21-1943-2025
Research article
 | 
12 Sep 2025
Research article |  | 12 Sep 2025

Regional modeling of internal-tide dynamics around New Caledonia – Part 2: Tidal incoherence and implications for sea surface height observability

Arne Bendinger, Sophie Cravatte, Lionel Gourdeau, Clément Vic, and Florent Lyard

Related authors

High-Latitude Eddy Statistics from SWOT assessed by in situ observations
Charly de Marez, Arne Bendinger, and Ahmad Fehmi Dilmahamod
EGUsphere, https://doi.org/10.5194/egusphere-2025-6055,https://doi.org/10.5194/egusphere-2025-6055, 2025
This preprint is open for discussion and under review for Ocean Science (OS).
Short summary
Hidden vortices: Near-equatorial low-oxygen extremes driven by high-baroclinic-mode vortices
Florian Schütte, Johannes Hahn, Ivy Frenger, Arne Bendinger, Fehmi Dilmahamod, Marco Schulz, and Peter Brandt
EGUsphere, https://doi.org/10.5194/egusphere-2025-2175,https://doi.org/10.5194/egusphere-2025-2175, 2025
Short summary
Internal-tide vertical structure and steric sea surface height signature south of New Caledonia revealed by glider observations
Arne Bendinger, Sophie Cravatte, Lionel Gourdeau, Luc Rainville, Clément Vic, Guillaume Sérazin, Fabien Durand, Frédéric Marin, and Jean-Luc Fuda
Ocean Sci., 20, 945–964, https://doi.org/10.5194/os-20-945-2024,https://doi.org/10.5194/os-20-945-2024, 2024
Short summary
Regional modeling of internal-tide dynamics around New Caledonia – Part 1: Coherent internal-tide characteristics and sea surface height signature
Arne Bendinger, Sophie Cravatte, Lionel Gourdeau, Laurent Brodeau, Aurélie Albert, Michel Tchilibou, Florent Lyard, and Clément Vic
Ocean Sci., 19, 1315–1338, https://doi.org/10.5194/os-19-1315-2023,https://doi.org/10.5194/os-19-1315-2023, 2023
Short summary
Eddy-enhanced primary production sustains heterotrophic microbial activities in the Eastern Tropical North Atlantic
Quentin Devresse, Kevin W. Becker, Arne Bendinger, Johannes Hahn, and Anja Engel
Biogeosciences, 19, 5199–5219, https://doi.org/10.5194/bg-19-5199-2022,https://doi.org/10.5194/bg-19-5199-2022, 2022
Short summary

Cited articles

Alford, M. H., MacKinnon, J. A., Nash, J. D., Simmons, H., Pickering, A., Klymak, J. M., Pinkel, R., Sun, O., Rainville, L., Musgrave, R., Beitzel, T., Fu, K. -H., Lu, C. -W.: Energy flux and dissipation in Luzon Strait: Two tales of two ridges, J. Phys. Oceanogr., 41, 2211–2222, https://doi.org/10.1175/JPO-D-11-073.1, 2011. a
Arbic, B. K.: Incorporating tides and internal gravity waves within global ocean general circulation models: A review, Prog. Oceanogr., 206, 102824, https://doi.org/10.1016/j.pocean.2022.102824, 2022. a, b
Arbic, B. K., Alford, M. H., Ansong, J. K., Buijsman, M. C., Ciotti, R. B., Farrar, J. T., Hallberg, R. W., Henze, C. E., Hill, C. N., Luecke, C. A., Menemenlis, D., Metzger, E. J., Muller, M., Nelson, A. D., Nelson, B. C., Ngodock, H. E., Ponte, R. M., Richman, J. G., Savage, A. C., Scott, R. B., Shriver, J. F., Simmons, H. L., Souopgui, I., Timko, P. G., Wallcraft, A. J., Zamudio, L., Zhao, Z.: Primer on global internal tide and internal gravity wave continuum modeling in HYCOM and MITgcm, New frontiers in operational oceanography, 307–392, http://purl.flvc.org/fsu/fd/FSU_libsubv1_scholarship_submission_1536242074_55feafcc (last access: 29 September 2021), 2018. a
Bella, A., Lahaye, N., and Tissot, G.: Internal tide energy transfers induced by mesoscale circulation and topography across the North Atlantic, J. Geophys. Res.-Oceans, 129, e2024JC020914, https://doi.org/10.1029/2024JC020914, 2024. a
Bendinger, A.: Internal tides around New Caledonia : dynamics, eddy-internal tide interactions, and SWOT observability, Theses, Université Paul Sabatier – Toulouse III, https://theses.hal.science/tel-04618408 (last access: 20 June 2024), 2023. a
Short summary
Temporal variability of the semidiurnal internal tide around New Caledonia is investigated using regional modeling. An important contribution to temporal variability not linked to the spring–neap tide cycle is due to the presence of mesoscale eddies both at the generation sites and in the propagation direction. The incoherent tide has a widespread signature in sea surface height (SSH), challenging the SSH observability of mesoscale to submesoscale dynamics.
Share