Articles | Volume 29, issue 2
https://doi.org/10.5194/npg-29-161-2022
Special issue:
https://doi.org/10.5194/npg-29-161-2022
Research article
 | 
07 Apr 2022
Research article |  | 07 Apr 2022

Estimate of energy loss from internal solitary waves breaking on slopes

Kateryna Terletska and Vladimir Maderich

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Cited articles

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Alford, M. N., Peacok, T., Mackinnon, J. A., and Tang, D.: The formation and fate of internal waves in the South China Sea, Nature, 521, 65–69, 2015. a
Apel, J. R., Ostrovsky, L. A., and Stepanyants, Y. A.: Internal solitons in the ocean, J. Acoust. Soc. Am., 98, 2863, https://doi.org/10.1121/1.414338, 1995. a
Bai, X., Lamb, K., Xu, J., and Liu, Z.: On Tidal Modulation of the Evolution of Internal Solitary-Like Waves Passing Through a Critical Point, J. Phys. Oceanogr., 51, 2533–2552, https://doi.org/10.1175/JPO-D-20-0167.1, 2021. a
Boegman, L. and Stastna, M.: Sediment Resuspension and Transport by Internal Solitary Waves, Annu. Rev. Fluid Mech., 51, 129–154, https://doi.org/10.1146/annurev-fluid-122316-045049, 2019. a
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Short summary
Internal solitary waves (ISWs) emerge in the ocean and seas in various forms and break on the shelf zones in a variety of ways. This results in intensive mixing that affects processes such as biological productivity and sediment transport. Mechanisms of wave interaction with slopes are related to breaking and changing polarity. Our study focuses on wave transformation over idealized shelf-slope topography using a two-layer stratification. Four types of ISW transformation over slopes are shown.
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