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- W2545083823 abstract "Gravity–capillary solitary waves are generated by a moving ‘air-suction’ forcing instead of a moving ‘air-blowing’ forcing. The air-suction forcing moves horizontally over the surface of deep water with speeds close to the minimum linear phase speed $c_{min}=23~text{cm}~text{s}^{-1}$ . Three different states are observed according to forcing speeds below $c_{min}$ . At relatively low speeds below $c_{min}$ , small-amplitude linear circular depressions are observed, and they move steadily ahead of and along with the moving forcing. As the forcing speed increases close to $c_{min}$ , however, nonlinear three-dimensional (3-D) gravity–capillary solitary waves are observed, and they move steadily ahead of and along with the moving forcing. Finally, when the forcing speed is very close to $c_{min}$ , oblique shedding phenomena of 3-D gravity–capillary solitary waves are observed ahead of the moving forcing. We found that all the linear and nonlinear wave patterns generated by the air-suction forcing correspond to those generated by the air-blowing forcing. The main difference is that 3-D gravity–capillary solitary waves are observed ‘ahead of’ the air-suction forcing whereas the same waves are observed ‘behind’ the air-blowing forcing." @default.
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- W2545083823 date "2016-10-27" @default.
- W2545083823 modified "2023-10-16" @default.
- W2545083823 title "Experimental observation of gravity–capillary solitary waves generated by a moving air suction" @default.
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- W2545083823 doi "https://doi.org/10.1017/jfm.2016.639" @default.
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