1. A unified normal modes approach to dynamic tides and its application to rotating stars with realistic structure
P. B. Ivanov and S. V. Chernov,
PN Lebedev Physical Institute
and
J. C. B. Papaloizou,
University of Cambridge

3. Dynamic versus quasi-static tides in the normal mode approach
There are two contributions, which can be separated by the requirement that wave-like phenomena play either major or minor role.
1) Quasi-static tides. These may be thought as due to excitation of normal modes with eigen frequencies much
larger than forcing frequencies. The energy and angular momentum are transferred to stars on a time scale of order of inverse forcing frequencies by viscous forces.
The main uncertainty is the value of “tidal Q” defined as
the ratio of the energy stored in tidal bulge to an
amount of energy dissipated per one orbital period.

4. Dynamic tides There are two types of dynamic tides:
1) the ones appropriate for highly eccentric orbits
(DT in the sense of Press and Teukolsky). During periastron passage normal modes of planet and stellar pulsations are exited. These are: fundamental modes with frequencies ~ *, g-modes in case of the presence stably stratified sizable regions as expected in stars, low frequency inertial waves with frequencies ~ , etc.
2) Dynamic tides in the sense of Zahn, operating
in rotating stars with any eccentricity. In this case it is assumed that eigen frequencies are of the same order as forcing frequencies. Energy and angular momentum are transferred to the star by the action of viscosity.

6. Dynamic tides operating in systems with periodic orbits
Let me assume that the orbit is strictly periodic. In this case
we can decompose all quantities of interest in Fourier series in
time:

7. It is assumed below that the modes have ‘dense’ spectrum (it is appropriate for, say, g-modes) and the resonance condition
is satisfied for a particular mode:
We will need an expression for the mode norm
where ξ is the mode eigen vector, and η ≈ ξ when viscosity
is small, and an expression for the mode coupling with
the perturbing potential.

8. Change of canonical energy

9. Overlap integrals
The forcing term can be represented as a product of two parts: the one determined by the amplitude of perturbing potential and the one describing properties of an individual resonant eigen mode. The latter term is called the overlap integral.

10. Regime of moderately large viscosity

11. Regime of very small viscosity

12. Analogous expressions for parabolic encounters

13. Evaluation of the overlap integrals, the case of sun-like stars
The overlap integrals can be evaluated analytically using the
WKBJ technique. This can be done in the so-called ‘traditional’
approximation for rotating stars. Calculations are especially simple
for sun-like stars with a radiative core and convective envelope.

18. New results for parabolic encounters
The strength of interaction is characterised by the transferred energy expressed in units
Gmp2/R*, where mp – is the perturber mass assumed to be one Jupiter from now on.
Additionally we plot evolution time scale
of semi-major axis as a function of orbital
period after circularisation.

23. Conclusions
In all tidal problems the overlap integrals play a fundamental role. Provided that the action of viscosity is specified they fully determine tidal interactions. The formalism based on the overlap integrals allows one to study tidal interactions in all possible regimes.
When either parabolic tidal encounters are considered or dynamic tides in the regime of moderately large viscosity it is enough to know the overlap integrals and eigen frequencies to calculate all quantities determining tidal interactions.
The transfer of energy as a result of tidal interaction is larger for stars having convective envelopes. Parabolic tidal encounters are also stronger for stars with smaller average density. Say, when a sun-like model is compared with a n=3 polytrope of the same mass and radius,
The transfer of energy is much larger in the case of stars with realistic structure when η is sufficiently large.