Astron. Astrophys. 361, 1127-1142 (2000)
Influence of the solar atmosphere on the p-mode eigenoscillations
N.S. Dzhalilov 1,
J. Staude 2 and
K. Arlt 2
1 Institute of Terrestrial Magnetism, Ionosphere and Radio Wave Propagation of the Russian Academy of Sciences, Troitsk City, Moscow Region, 142092, Russia (namig@izmiran.rssi.ru)
2 Astrophysikalisches Institut Potsdam, Sonnenobservatorium Einsteinturm, 14473 Potsdam, Germany (jstaude, karlt@aip.de)
Received 12 April 2000 / Accepted 8 August 2000
Abstract
An asymptotic theory of global adiabatic p-modes is
developed, taking into account the influence of the solar atmosphere.
It is shown that waves of the whole frequency range
mHz may reach the
chromosphere-corona transition region (CCTR) by means of a tunneling
through the atmospheric barriers. The primary acoustic cavity inside
the Sun becomes considerably extended by this way, leading to a change
of frequencies: low frequencies are increased, while high frequencies
are decreased. The transition from low p-mode frequencies to
high peak frequencies mHz) is
smooth.
The locations of the turning points are determined from the wave
equation for . It is shown that the
internal turning point of the acoustic cavity is strongly shifted
toward the center of the Sun, while the upper turning point is shifted
from the surface to CCTR. That means, the turning points cannot be
located in the convective zone. A new complex integral dispersion
relation for the eigenfrequencies is derived. The imaginary parts of
the frequencies indicate a decay of the amplitudes, resulting from
considerable energy losses by tunneling from the main cavity.
It is shown that waves with a decaying amplitude (complex
frequency) may exist in a limited area only, penetration of linear
p-modes to the corona is impossible. The CCTR acts as a free
surface. We conclude that the p-modes may drive forced surface
gravity waves at this surface.
Key words: hydrodynamics
Sun:
oscillations
Sun: interior
Sun: atmosphere
Send offprint requests to: J. Staude
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Contents
© European Southern Observatory (ESO) 2000
Online publication: October 10, 2000
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