Nonlinear magneto-acoustic waves in the solar atmosphere

2001 ◽  
Vol 34 (2-4) ◽  
pp. 399-409
Author(s):  
César A. Mendoza-Briceño ◽  
Miguel H. Ibáñez ◽  
Valery M. Nakariakov
1990 ◽  
Vol 142 ◽  
pp. 231-235
Author(s):  
P. Ulmschneider

Turbulent surface convection zones of stars generate acoustic waves which contribute to the heating of chromospheres and coronae. The dissipation of limiting strength acoustic shock waves agrees well with the empirically determined chromospheric radiation loss rates. Acoustic waves with frequency and energy required for the chromospheric heating are observed in the solar atmosphere. Acoustic heating can explain the basal chromospheric emission of slowly rotating stars and constitutes a weak background in faster rotating stars; it can not explain the emission-rotation correlation and the surface variation of emission which are due to magnetic heating.


Author(s):  
Robert Erdélyi

Can the ubiquitously magnetic solar atmosphere have any effect on solar global oscillations? Traditionally, solar atmospheric magnetic fields are considered to be somewhat less important for the existence and characteristic features of solar global oscillations ( p , f and the not-yet-observed g -modes). In this paper, I demonstrate the importance of the presence of magnetism and plasma dynamics for global resonant oscillations in the solar atmosphere. In particular, in the lower part of the solar atmosphere there are both coherent and random components of magnetic fields and velocity fields, each of which contribute on its own to the line widths and frequency variations of solar global acoustic waves. Changes in the coherent large-scale atmospheric magnetic fields cause frequency shifts of global oscillations over a solar cycle. The random character of the continuously emerging, more localized, magnetic carpet (i.e. small-scale, possibly even sub-resolution, loops) gives rise to additional frequency shifts. On the other hand, random and organized surface and sub-surface flows, like surface granulation, meridional flows or differential rotation, also affect the coupling mechanism of global oscillations to the lower magnetic atmosphere. The competition between magnetic fields and flows is inevitable. Finally, I shall discuss how solar global oscillations can resonantly interact with the overlaying inhomogeneous lower solar atmosphere embedded in a magnetic carpet. Line width broadening and distorsion of global acoustic modes will be discussed. The latter is suggested to be tested and measured by using ring-analysis techniques.


2007 ◽  
Vol 328 (3-4) ◽  
pp. 211-214 ◽  
Author(s):  
M. Haberreiter ◽  
W. Finsterle ◽  
S. M. Jefferies

2012 ◽  
Vol 38 (6) ◽  
pp. 388-393 ◽  
Author(s):  
N. S. Petrukhin ◽  
E. N. Pelinovsky ◽  
E. K. Batsyna

1988 ◽  
Vol 123 ◽  
pp. 439-442 ◽  
Author(s):  
F.-L. Deubner ◽  
M. Reichling ◽  
R. Langhanki

The amount of energy carried in the solar atmosphere by short period acoustic waves is particularly uncertain in the range of frequencies (ν ≥ 10mHz) which is potentially relevant for acoustic heating.


2009 ◽  
Vol 508 (2) ◽  
pp. 941-950 ◽  
Author(s):  
N. Bello González ◽  
M. Flores Soriano ◽  
F. Kneer ◽  
O. Okunev

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