“…The coupling between barotropic tidal waves at the sea surface and internal gravity waves facilitates heat and material exchange between the uppermost and deeper layers (Garrett, 2003;Lelong and Kunze, 2013;Morozov, 2018;Vic et al, 2019;Rippeth and Green, 2020;Stanev and Ricker, 2020). This largely interconnected dynamic is particularly pertinent in semi-enclosed basins, bays, and fjords with density profiles characterized by sharp gra-dients (Rattray, 1960;Niiler, 1968;Bell, 1975;Stigebrandt, 1980;Stigebrandt and Aure, 1989;Chapman and Giese, 1990;Münnich, 1996;Parsmar and Stigebrandt, 1997;Stigebrandt, 1999;Imberger, 2001, 2003;Inall et al, 2004;Cushman-Roisin et al, 2005;Johnsson et al, 2007;Boegman and Ivey, 2012;Park et al, 2016;Staalstrøm and Røed, 2016;Castillo et al, 2017;Roget et al, 2017;Stanev and Ricker, 2020;Xue et al, 2020).…”