Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Application to the Southern Ocean

By M. Nikurashin, Raffaele Ferrari. 2010

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View Paper: https://www.semanticscholar.org/paper/cef2f1ece64c61e828007f2048ba81f87bb624b1

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Citations in the corpus

Radiation and Dissipation of Internal Waves Generated by Geostrophic Motions Impinging on Small-Scale Topography: Theory (2010, methodology): “A quantitative comparison using more realistic model configurations is the focus of a companion paper (Nikurashin and Ferrari 2010, hereafter NF) where we show, using multibeam topography, velocity, and stratification data available for the SO, that the parameter space described here is relevant to…”
Concurrent Simulation of the Eddying General Circulation and Tides in a Global Ocean Model (2010, unknown): “In AGHS and SHA a typical midlatitude stratification was used throughout the entire globe, and internal tide activity in some polar regions (for instance, the Scotia Sea) was almost certainly artificially high (Padman et al., 2006).”
Global energy conversion rate from geostrophic flows into internal lee waves in the deep ocean (2011, background): “It is believed that the eddy field in turn loses its energy through friction in bottom boundary layers [Arbic and Flierl, 2004] and along western boundaries [Zhai et al., 2010], and through internal wave generation at rough topography [Nikurashin and Ferrari, 2010a].”
Spatial and temporal variability of global ocean mixing inferred from Argo profiles (2012, background): “…interacting with the high concentration of eddies [Padman et al., 1990; Kunze, 1995], internal waves generated from topographyeddy interactions [Nikurashin and Ferrari, 2010; Liang and 5 of 6 Thurnherr, 2012], or due to incorrectly identifying the strain associated with the eddies as internal…”
Overturning circulation driven by breaking internal waves in the deep ocean (2013, methodology): “…mixing locally, from the 30% value used by St. Laurent et al. [2002] to 50%, a value suggested by idealized numerical simulations for lee waves [Nikurashin and Ferrari, 2010a; Nikurashin and Ferrari, 2010b], increases the maximum of the water-mass transformation driven by lee wave-driven…”