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Volumn 272, Issue 5266, 1996, Pages 1296-1300

The seismic structure of the sun

(26)  Gough, D O a   Kosovichev, A G b   Toomre, J c   Anderson, E d   Antia, H M e   Basu, S f   Chaboyer, B g   Chitre, S M e   Christensen Dalsgaard, J f   Dziembowski, W A h   Eff Darwich, A i   Elliott, J R a   Giles, P M b   Goode, P R j   Guzik, J A k   Harvey, J W d   Hill, F d   Leibacher, J W d   Monteiro, M J P F G l   Richard, O m   more..


Author keywords

[No Author keywords available]

Indexed keywords

CONVECTION ZONE; EQUATION OF STATE; GLOBAL OSCILLATION NETWORK GROUP; OPACITY; SEISMIC STRUCTURE; WAVE MOTION;

EID: 0029756839     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.272.5266.1296     Document Type: Article
Times cited : (192)

References (57)
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    • Frequencies also depend on the variation of density but to a lesser extent than they depend on sound speed [see (9)].
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    • That time is inversely proportional to the magnitude of the group velocity and is directly proportional to the relative density of ray-path segments.
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    • This technique has been carried out with only asymptotic representations of the resonance conditions [for example, see J. Christensen-Dalsgaard et al., Nature 315, 378 (1985)].
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    • i divided by the modal inertia, which is the functional form of any surface uncertainty [see (3)].
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    • That sets the radius of the base of the adiabatically stratified part of the convection zone at about 0.709R. This value is somewhat less than the value 0.713R obtained previously by J. Christensen-Dalsgaard, D. O. Gough, and M, J. Thompson [Astrophys. J. 378, 413 (1991)], and by A. G. Kosovichev and A. V. Fedorova [Sov. Astron. 35, 507 (1991)]. A study of the transition at the base of the convection zone [see (30)] is consistent with the new result, although a repeat of the analysis with the use of the reference models of Richard et al. (15) yields 0.714R.
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    • That sets the radius of the base of the adiabatically stratified part of the convection zone at about 0.709R. This value is somewhat less than the value 0.713R obtained previously by J. Christensen-Dalsgaard, D. O. Gough, and M, J. Thompson [Astrophys. J. 378, 413 (1991)], and by A. G. Kosovichev and A. V. Fedorova [Sov. Astron. 35, 507 (1991)]. A study of the transition at the base of the convection zone [see (30)] is consistent with the new result, although a repeat of the analysis with the use of the reference models of Richard et al. (15) yields 0.714R.
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    • 2 tends to be associated with corresponding relative decreases in ρ and μ.
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    • We have investigated the structure of the transition between the convection zone and the radiative interior by first considering how mode frequency varies with the phase difference between the surface of the sun and the base of the convection zone, after having filtered out surface effects, and then comparing it with theoretical models (32). The signature of the transition oscillates with phase, in step with the eigenfunctions, with an amplitude that is smaller than that of the reference model, confirming that, if spherical, the transition is smoother than that of the model. The apparent smoothness might have come about because what has been observed is actually the spherical average of an aspherical structure. Adiabatic convective overshooting is likely to increase the amplitude; therefore, if such overshooting occurs in the sun, the physical discrepancy is actually greater than It appears at first sight. There is some indication that the amplitude of the oscillatory signal varies with the ratio m/( of azimuthal order to degree. This suggests that the structure of the lower boundary layer of the convection zone might vary with latitude. Although at present this is no more than a hint, it points to an exciting direction of research with further longterm seismic data.
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    • note
    • GONG is managed by the National Solar Observatory, a division of the National Optical Astronomy Observatories, operated by AURA under a cooperative agreement with NSF. We acknowledge financial support from the U.K. Particle Physics and Astronomy Research Council, NSF, NASA, and Danmarks Gruncfforskningsfond.


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