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The Kelvin Wake: Why Every Ship Draws the Same Angle

Why deep-water wave dispersion locks every ship wake to a fixed 19.47° half-angle, what the transverse and diverging wave families are, and why shallow water breaks the rule.

mysimulator teamUpdated June 2026≈ 7 min read▶ Open the simulation

Every moving ship writes the same angle on the water

Watch any ship, duck or water strider moving across deep, calm water and its wake forms the same V-shaped pattern, bounded by an angle that does not depend on speed, size or shape: 19.47° on either side of the direction of travel, for a total wake angle of 38.94°. Lord Kelvin worked this out in 1887 from pure wave-dispersion physics, and the constancy of that angle — regardless of how fast the disturbance moves — is one of the more surprising results in classical fluid mechanics.

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Deep-water waves are dispersive

The whole effect follows from one fact: on deep water, surface gravity waves of different wavelengths travel at different speeds. Longer waves travel faster, following the deep-water dispersion relation:

c(λ) = sqrt( g·λ / (2π) )     (phase speed of a deep-water wave)

g = gravitational acceleration, λ = wavelength

A moving hull or bow disturbance excites waves of essentially every wavelength and direction. Each wave component then travels off at its own speed and direction, and stays coherent with (interferes constructively with) its neighbours only where the geometry lines up — everywhere else the many different wavelengths fall out of phase and cancel. What survives that cancellation is not a random mess but a very specific, sharply bounded pattern.

Two families of waves inside the wake

Constructive interference survives in two distinct families. Transverse waves run roughly perpendicular to the direction of travel, trailing directly behind the source, with crests that curve backward as you move outward from the centreline. Diverging waves radiate outward at a shallower angle from the source track, with crests roughly perpendicular to their own direction of travel rather than to the ship's heading. Both families exist everywhere inside the wake envelope, and it is their combined crest pattern — including a signature cusp where the transverse and diverging crests meet at the wake's edge — that gives a ship wake its distinctive feathered look.

Where the 19.47° comes from

The angle is a stationary-phase result: for a disturbance moving at constant velocity, group velocity being exactly half the phase velocity for deep-water waves (a direct consequence of the dispersion relation above) constrains every constructively-interfering wave component to lie within a wedge whose half-angle works out to arcsin(1/3) ≈ 19.47°, independent of source speed. A supertanker and a duck produce wake angles that are, in the deep-water limit, geometrically identical — only the wavelengths, amplitudes and overall scale of the pattern differ, which is a genuinely counter-intuitive result the first time you see the derivation.

Where the theory breaks: shallow water and high speed

The constant 19.47° angle assumes deep water — depth much greater than the relevant wavelengths — and a source that is not moving unreasonably fast relative to the natural wave speeds available at that depth. In shallow water, wave speed becomes depth-limited rather than wavelength-limited, and a vessel approaching or exceeding that shallow-water wave speed produces a narrower wake angle than 19.47°, collapsing toward a Mach-cone-like pattern at high enough Froude number — the same physics, structurally, as the sonic boom cone behind a supersonic aircraft, with the depth-limited wave speed playing the role of the sound speed. This shallow-water narrowing has practical consequences: fast ferries in coastal shipping lanes must be operated carefully because their wake angle and wave energy distribution both change once they cross into the shallow-water regime.

Frequently asked questions

Why is the Kelvin wake angle always about 19.47° no matter how fast the ship goes?

The angle comes from a stationary-phase argument built on the deep-water wave dispersion relation, where group velocity is always exactly half the phase velocity. That ratio, not the ship's actual speed, is what fixes the wedge angle at arcsin(1/3) ≈ 19.47°, so the geometry is identical for a duck and for an aircraft carrier in deep water.

What is the difference between the transverse and diverging waves in a wake?

Transverse waves trail roughly perpendicular to the direction of travel with crests curving backward off the centreline, while diverging waves radiate outward at a shallower angle with crests aligned closer to their own direction of propagation. Both are present everywhere inside the wake envelope and together produce the feathered pattern with a cusp where they meet.

Does the 19.47° angle still hold in shallow water or at very high speed?

No — that value assumes deep water, where wave speed depends only on wavelength. In shallow water wave speed becomes depth-limited, and a vessel moving near or above that limiting speed produces a narrower wake angle, eventually collapsing into a Mach-cone-like pattern analogous to a supersonic aircraft's sonic boom cone.

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Everything above runs in your browser — open Kelvin Ship Wake and change the parameters while it is running. Nothing is installed, nothing is uploaded, the whole model lives in one tab.

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