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Eric Kunze and Ren-Chieh Lien

( x , y ) ( Nikurashin et al. 2014 ; Trossman et al. 2015 , 2016 ), although Klymak (2018) reported that blocking and hydraulic effects from larger-scale topography ( k < f / U ) dominated near-bottom dissipation by factors of 2–3; (ii) microstructure sampling biases in a highly heterogeneous turbulence field ( Waterman et al. 2014 ; Klymak 2018 ); (iii) internal wave–wave interactions transferring energy into waves free to propagate out of the jets ( f < ω E < N ); and (iv) advection

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