For implicit methods, various approximations to the
square root in oneway.3d lead to approximate equations
of different orders of accuracy.
For downward continuation in Cartesian coordinates,
those methods are known by their respective angular
accuracy as the
equation,
equation and so on.
Although the meanings of
,
are
undefined in ray coordinates where the extrapolation axis
is time, we can still write approximations for
the numerical finite-difference solutions using analogous
approximations.
With the notation
| (18) |
| |
(19) |
A simple way of deriving the
equation is by a
second-order Taylor series expansion of the extrapolation
wavenumber
function of the variables
and
: ,
=0,=0 +
. |_0 +
. |_0 +
+
12 . |_0 ^2 +
. |_0 +
12 . |_0 ^2 .
Introducing oneway.3d.b into taylor.3d, we obtain
an equivalent form for the
equation in a
semi-orthogonal 3D Riemannian space:
i 2 + k_o
+ i2 k_o
+ 12 k_o 2 k_o^2- ^2
+ i2 k_o
+ 12 k_o 2 k_o^2 -^2
+ 12 k_o 2^2 k_o^2 -.
fifteen.3d specialized for the case of 2D coordinate systems obtained by ray tracing is further discussed in Appendix A.
For the particular case of Cartesian coordinates
(
),
| (20) |