The starting point for the discussion of the ray tracing is given by the acoustic wave equation,
which in the case of a watercolumn with a constant density can be written as
 |
(2.1) |
where
stands for the pressure of the acoustic wave,
represents the signal transmitted by the acoustic source,
represents the source position and
represents the nabla differential operator.
Applying a Fourier transform to both sides of Eq.(2.1) one can obtain
the so called Helmholtz equation:
 |
(2.2) |
where
and
Let's consider a plane wave-like approximation to the solution of Eq.(2.2)
and write that [4]
 |
(2.3) |
where
represents a slowly changing wave amplitude,
and
stands for a rapidly evolving phase;
the surfaces with constant
represent the wavefronts;
analogously,
the surfaces with constant
are called timefronts.
By placing Eq.(2.3) into the homogeneous form of Eq.(2.2),
considering the high frequency approximation
(where
) and separating the real and imaginary terms of the equation,
one can obtain the Eikonal equation:
 |
(2.4) |
and the transport equation:
 |
(2.5) |
The following sections will describe the solution of Eqs.(2.4)-(2.5).
Orlando Camargo Rodríguez
2012-06-21