Reply to comment by M. Ortega-Sánchez et al. on “High-angle wave instability and emergent shoreline shapes : 1. Modeling of sand waves, flying spits, and capes”
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Author Posting. © American Geophysical Union, 2008. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 113 (2008): F01006, doi:10.1029/2007JF000885.
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On nonhydrostatic coastal model simulations of shear instabilities in a stratified shear flow at high Reynolds number Zhou, Zheyu; Yu, Xiao; Hsu, Tian-Jian; Shi, Fengyan; Geyer, W. Rockwell; Kirby, James T. (John Wiley & Sons, 2017-04-11)The nonhydrostatic surface and terrain-following coastal model NHWAVE is utilized to simulate a continually forced stratified shear flow in a straight channel, which is a generic problem to test the existing nonhydrostatic ...
High-angle wave instability and emergent shoreline shapes : 1. Modeling of sand waves, flying spits, and capes Ashton, Andrew D.; Murray, A. Brad (American Geophysical Union, 2006-12-15)Contrary to traditional findings, the deepwater angle of wave approach strongly affects plan view coastal evolution, giving rise to an antidiffusional “high wave angle” instability for sufficiently oblique deepwater waves ...
Brink, Kenneth H.; Cherian, Deepak A. (Sears Foundation for Marine Research, 2013-11-01)Finite amplitude instability of an idealized tidal mixing front is considered for cases where there is an active symmetric instability during the early stages of evolution. This can happen either when the initial front is ...