Titlebook: Breaking Waves; IUTAM Symposium Sydn Michael L. Banner,Roger H. J. Grimshaw Conference proceedings 1992 Springer-Verlag, Berlin Heidelberg

強(qiáng)所

Breaking Wave Statistics Obtained During ‘Swade’published field measurements of breaking wave statistics, using different techniques, can be encompassed nicely by the present void fraction statistics in a more meaningful and orderly way. The frequency, or number fraction, of breaking waves levels off as the wind speed increases.

Magnificent

Conference proceedings 1992 technological importance, A familiar illustration is provided with white-capping and microbreaking of the wind-driven ocean sUrface waves, which is believed to play an important part in the transfers of momentum, mass and heat across the air-sea interface, as well as in the production of underwater

DALLY

Reporting Standards for Literature Reviewsrgy transfer between the waves in the equilibrium range and those at the spectral peak, involving both upward and downward cascading of the wave energy. The variation of z. directly reflects the degree of over- and under-saturation of the level of the equilibrium range.

辯論的終結(jié)

平

https://doi.org/10.1007/978-1-4614-1545-9o intensive observational scrutiny. These include: changes in microwave reflectivity; stress and gas transfer enhancement; formation of bubble clouds and sound generation; dissipation of surface waves.

GOUGE

Plural Identities in the Age of Nationalismsme phase speed. The dynamical theory of the generation of parasitic capillaries has been developed by Longuet-Higgins (1963), Crapper (1970) and Ruvinsky et al. (1981, 1985, 1991). This so far takes into account only the first-order effects of viscous damping.

性冷淡

偏見

領(lǐng)袖氣質(zhì)

The Physical Consequences of Wave Breaking in Deep Waterion on the ocean surface. In particular, the complex process of wave breaking has a wide range of consequences for remote sensing, momentum, heat and mass transfer and oceanic acoustics. In this paper we consider some of the more important effects of wave breaking that have recently been subjected t

下邊深陷

Capillary Rollers and Bores the forward face of moderately short gravity waves, especially those with wavelengths 5 to 50 cm; see Figure la. These capillary waves were first studied experimentally by Cox (1958). Evidently their existence depends on the fact that a gravity wave and a much shorter capillary wave may have the sa