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Asymptotic expansion for small
values.
In this section we perform the small
calculations of Sec. VI.
We start from the kinetic equation written as Eq. (40). There
we change variables in the first line of
Eq. (40) as
and in the second line of Eq. (40) as
Then the Eq. (40) becomes the following form:
Here we introduced integrand
and
to be
 |
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 |
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(14) |
Before proceeding, note the following symmetry:
and
To quantify the contribution of near-inertial waves to a
mode, we write
Subsequently, in the domain (a) we write
in
, and
in
.
Furthermore, we expand
and
in powers of
and
without making any assumptions of the relative
smallness of
and
.
We use the facts that
Define
and
This allows us to expand
,
,
and
in powers of
and
.
We perform these calculations on
Mathematica using Series command, and extensively using Assumptions field in the FullSimplify command.
Mathematica was then able to
perform the integrals of
and
over
from
to
in (C1) analytically. The result is given by
Eq. (41).
Next: Bibliography
Up: Oceanic Internal Wave Field:
Previous: Frequency-vertical-wavenumber and horizontal-vertical-wavenumber spectrum
Dr Yuri V Lvov
2008-07-08