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Retrograde waves with frequencies much lower than the rotation frequency
become trapped in the solar radiative interior. The eigenfunctions of the
compressible, nonadiabatic (ϵ-mechanism and radiative losses taken
into account) Rossby-like modes are obtained by an asymptotic method assuming
a very small latitudinal gradient of the rotation rate. An integral
dispersion relation for the complex eigenfrequencies is derived as a
solution of the boundary value problem. The discovered resonant cavity modes
(called R-modes) are fundamentally different from the known r-modes:
their frequencies are functions of the solar interior structure, and the
reason for their existence is not related to geometrical effects. The most
unstable R-modes are those with periods of ≈1–3 yr, 18–30 yr,
and 1500–20 000 yr; these three separate period ranges are known from
solar and geophysical data. The growing times of those modes which are
unstable with respect to the ϵ-mechanism are ≈
102,103,
and 105 years, respectively. The amplitudes of the R-modes are growing
towards the center of the Sun. We discuss some prospects to develop the
theory of R-modes as a driver of the dynamics in the convective zone which
could explain, e.g., observed short-term fluctuations of rotation, a control
of the solar magnetic cycle, and abrupt changes of terrestrial climate in the
past
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