Articles | Volume 22, issue 4
https://doi.org/10.5194/os-22-2249-2026
https://doi.org/10.5194/os-22-2249-2026
Research article
 | 
27 Jul 2026
Research article |  | 27 Jul 2026

Bottom topography effects on the internal wave climate in the Ionian Sea

Florian Kokoszka, Stefania Sparnocchia, Davide Cavaliere, Vincenzo Artale, Mireno Borghini, Beatrice Giambenedetti, and Federico Falcini

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Cited articles

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Artale, V., Falcini, F., Marullo, S., Bensi, M., Kokoszka, F., Iudicone, D., and Rubino, A.: Linking mixing processes and climate variability to the heat content distribution of the Eastern Mediterranean abyss, Sci. Rep., 8, 1–10, https://doi.org/10.1038/s41598-018-29343-4, 2018. 
Bellacicco, M., Anagnostou, C., Falcini, F., Rinaldi, E., Tripsanas, K., and Salusti, E.: The 1987 Aegean dense water formation: A streamtube investigation by comparing theoretical model results, satellite, field, and numerical data with contourite distribution, Mar. Geol., 375, 120–133, https://doi.org/10.1016/j.margeo.2016.01.012, 2016. 
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Short summary
The deep Ionian Sea strongly influences how the Mediterranean water masses circulate. By studying how internal waves interact with the seafloor, we found that rougher terrain changes how wave energy is spread out. Energy shifts from large to small scales, affecting deep water mixing. These findings help improve models of Mediterranean circulation by showing how seafloor shape impacts mixing in the deep sea.
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