Capillary wave
A capillary wave is a wave traveling along the phase boundary of a fluid, whose dynamics and phase velocity are dominated by the effects of surface tension. Capillary waves are common in nature, and are often referred to as ripples. The wavelength of capillary waves on water is typically less than a few centimeters, with a phase speed in excess of 0.2–0.3 meter/second. A longer wavelength on a fluid interface will result in gravity–capillary waves which are influenced by both the effects of surface tension and gravity, as well as by fluid inertia. Ordinary gravity waves  have a still longer wavelength. When generated by light wind in open water, a nautical name for them is cat's paw waves. Light breezes which stir up such small ripples are also sometimes referred to as cat's paws. On the open ocean, much larger ocean surface waves (seas and swells) may result from coalescence of smaller wind-caused ripple-waves. Dispersion relation. The dispersion relation describes the relationship between wavelength and frequency in waves. Distinction can be made between pure capillary waves – fully dominated by the effects of surface tension – and gravity–capillary waves which are also affected  by gravity. Capillary waves, proper. The dispersion relation for capillary waves is where formula_2 is the angular frequency, formula_3 the surface tension, formula_4 the density of the heavier fluid, formula_5 the density of the lighter fluid and formula_6 the wavenumber. The wavelength is formula_7 For the boundary between fluid and vacuum (free surface), the dispersion relation reduces to Gravity–capillary waves. In general, waves are also affected by gravity and are then called gravity–capillary waves. Their dispersion relation reads, for waves on the interface between two fluids of infinite depth: where formula_10 is the acceleration due to gravity, formula_4  and formula_5 are the mass density of the two fluids formula_13. The factor formula_14 in the first term is the Atwood number. Gravity wave regime. For large wavelengths (small formula_15), only the first term is relevant and one has gravity waves. In this limit, the waves have a group velocity half the phase velocity: following a single wave's crest in a group one can see the wave appearing at the back of the group, growing and finally disappearing at the front of the group. Capillary wave regime. Shorter (large formula_6) waves (e.g. 2 mm for the water–air interface ), which are proper capillary waves, do the opposite: an individual wave appears at the front of the group, grows when moving towards the group center and finally disappears at the back of the group. Phase velocity is two thirds of group velocity in this limit. Phase velocity minimum. Between these two limits is a point at which the dispersion caused by gravity cancels out the dispersion due to the capillary effect. At a certain wavelength, the group velocity equals the phase velocity, and there is no dispersion. At precisely this same wavelength, the phase velocity of gravity–capillary waves as  a function of wavelength (or wave number) has a minimum. Waves with wavelengths much smaller than this critical wavelength formula_17 are dominated by surface tension, and much above by gravity. The value of this wavelength and the associated minimum phase speed formula_18 are: For the air–water interface, formula_17 is found to be , and formula_18 is . If one drops a small stone or droplet into liquid, the waves then propagate outside an expanding circle of fluid at rest; this circle is a caustic which corresponds to the minimal group velocity. Derivation. As Richard Feynman put it, ""[water waves] that are  easily seen by everyone and which are usually used as an example of waves in elementary courses [...] are the worst possible example [...]; they have all the complications that waves can have."" The derivation of the general dispersion relation is therefore quite involved. There are three contributions to the energy, due to gravity, to surface tension, and to hydrodynamics. The first two are potential energies, and responsible for the two terms inside the parenthesis, as is clear from the appearance of formula_10 and formula_3. For gravity, an assumption is made of the density of the fluids being constant (i.e., incompressibility), and  likewise formula_10 (waves are not high enough for gravitation to change appreciably). For surface tension, the deviations from planarity (as measured by derivatives of the surface) are supposed to be small. For common waves both approximations are good enough. The third contribution involves the kinetic energies of the fluids. It is the most complicated and calls for a hydrodynamic framework. Incompressibility is again involved (which is satisfied if the speed of the waves is much less than the speed of sound in the media), together with the flow being irrotational – the flow is then potential. These are typically also good  approximations for common situations. The resulting equation for the potential (which is Laplace equation) can be solved with the proper boundary conditions. On one hand, the velocity must vanish well below the surface (in the "deep water" case, which is the one we consider, otherwise a more involved result is obtained, see Ocean surface waves.) On the other, its vertical component must match the motion of the surface. This contribution ends up being responsible for the extra formula_6 outside the parenthesis, which causes all regimes to be dispersive, both at low values of formula_6, and high ones (except around the  one value at which the two dispersions cancel out.)