A ship moving with constant speed
on deep water generates a surface gravity
wave. In a reference frame where the ship is at rest we use polar coordinates
and
with
in the direction of the velocity of the water
relative to the ship. Then with
denoting the acceleration due to gravity,
the wave height is approximately given by
where
The integral is of the form of the real part of (36.12.1) with
,
,
,
, and
When
, that is, everywhere except close to the ship, the integrand
oscillates rapidly. There are two stationary points, given by
These coalesce when
This is the angle of the familiar V-shaped wake. The wake is a caustic of the
“rays” defined by the dispersion relation (“Hamiltonian”) giving the
frequency
as a function of wavevector
:
Here
, and
is the ship velocity
(so that
).
The disturbance
can be approximated by the method of uniform
asymptotic approximation for the case of two coalescing stationary points
(36.12.11), using the fact that
are real for
and complex for
. (See also §2.4(v).)
Then with the definitions
(36.12.12), and the real functions
the disturbance is

See Figure 36.13.1.