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Volumn 272, Issue 5266, 1996, Pages 1286-1292

The current state of solar modeling

Author keywords

[No Author keywords available]

Indexed keywords

GLOBAL OSCILLATION NETWORK GROUP; HELIOSEISMOLOGY; STELLAR STRUCTURE;

EID: 0029750056     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.272.5266.1286     Document Type: Article
Times cited : (1124)

References (124)
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    • Models of the evolution of solar internal rotation assume loss of angular momentum from the convection zone through the solar wind, the coupling to the interior taking place through various types of instability [A. S. Endal and S. Sofia, Astrophys. J 243, 625 (1981); M. H. Pinsonneault, S. D. Kawaler, S. Sofia, P. Demarque, ibid. 338, 424 (1989)]. These models have been useful in interpreting rotational velocities and lithium abundances in stellar clusters and in field stars near the main sequence. When applied to the sun, they fail to reproduce the near-uniform rotation of the present solar interior, as inferred from hellioseismology (1), indicating that other physical mechanisms must contribute to the solar internal spin-down.
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    • Models of the evolution of solar internal rotation assume loss of angular momentum from the convection zone through the solar wind, the coupling to the interior taking place through various types of instability [A. S. Endal and S. Sofia, Astrophys. J 243, 625 (1981); M. H. Pinsonneault, S. D. Kawaler, S. Sofia, P. Demarque, ibid. 338, 424 (1989)]. These models have been useful in interpreting rotational velocities and lithium abundances in stellar clusters and in field stars near the main sequence. When applied to the sun, they fail to reproduce the near-uniform rotation of the present solar interior, as inferred from hellioseismology (1), indicating that other physical mechanisms must contribute to the solar internal spin-down.
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    • The depth of the solar convection zone has been determined from helioseismic inversion to be (28.7 ± 0.3)% of the solar radius [J. Christensen-Dalsgaard, D. O. Gough, M. J. Thompson, Astrophys. J. 378, 413 (1991); A. G. Kosovichev and A. V. Fedorova, Astron. Zh. 68, 1015 (1991)].
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    • L. Biermann [Z Astrophys. 5, 117 (1932)] and T. G. Cowling [Mon. Not. R Astron. Soc. 96, 42 (1935)] were among the first to use mixing-length treatments to describe the transport of energy by convection. For a refined version, now commonly used, see E. Böhm-Vitense, Z. Astrophys. 46, 108 (1958); see (58) for an alternative, more recent formulation. Also, hydrodynamical simulations are now able to guide solar modelers [for example, R. F. Stein and Å Nordlund, Astrophys. J. 342, L95 (1989); N. Brummell, F. Cattaneo, J. Toomre, Science 269, 1370 (1995); Y.-C. Kim, P. A. Fox, S. Sofia, P. Demarque, Astrophys. J. 442, 422 (1995)].
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    • L. Biermann [Z Astrophys. 5, 117 (1932)] and T. G. Cowling [Mon. Not. R Astron. Soc. 96, 42 (1935)] were among the first to use mixing-length treatments to describe the transport of energy by convection. For a refined version, now commonly used, see E. Böhm-Vitense, Z. Astrophys. 46, 108 (1958); see (58) for an alternative, more recent formulation. Also, hydrodynamical simulations are now able to guide solar modelers [for example, R. F. Stein and Å Nordlund, Astrophys. J. 342, L95 (1989); N. Brummell, F. Cattaneo, J. Toomre, Science 269, 1370 (1995); Y.-C. Kim, P. A. Fox, S. Sofia, P. Demarque, Astrophys. J. 442, 422 (1995)].
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    • L. Biermann [Z Astrophys. 5, 117 (1932)] and T. G. Cowling [Mon. Not. R Astron. Soc. 96, 42 (1935)] were among the first to use mixing-length treatments to describe the transport of energy by convection. For a refined version, now commonly used, see E. Böhm-Vitense, Z. Astrophys. 46, 108 (1958); see (58) for an alternative, more recent formulation. Also, hydrodynamical simulations are now able to guide solar modelers [for example, R. F. Stein and Å Nordlund, Astrophys. J. 342, L95 (1989); N. Brummell, F. Cattaneo, J. Toomre, Science 269, 1370 (1995); Y.-C. Kim, P. A. Fox, S. Sofia, P. Demarque, Astrophys. J. 442, 422 (1995)].
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    • L. Biermann [Z Astrophys. 5, 117 (1932)] and T. G. Cowling [Mon. Not. R Astron. Soc. 96, 42 (1935)] were among the first to use mixing-length treatments to describe the transport of energy by convection. For a refined version, now commonly used, see E. Böhm-Vitense, Z. Astrophys. 46, 108 (1958); see (58) for an alternative, more recent formulation. Also, hydrodynamical simulations are now able to guide solar modelers [for example, R. F. Stein and Å Nordlund, Astrophys. J. 342, L95 (1989); N. Brummell, F. Cattaneo, J. Toomre, Science 269, 1370 (1995); Y.-C. Kim, P. A. Fox, S. Sofia, P. Demarque, Astrophys. J. 442, 422 (1995)].
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    • L. Biermann [Z Astrophys. 5, 117 (1932)] and T. G. Cowling [Mon. Not. R Astron. Soc. 96, 42 (1935)] were among the first to use mixing-length treatments to describe the transport of energy by convection. For a refined version, now commonly used, see E. Böhm-Vitense, Z. Astrophys. 46, 108 (1958); see (58) for an alternative, more recent formulation. Also, hydrodynamical simulations are now able to guide solar modelers [for example, R. F. Stein and Å Nordlund, Astrophys. J. 342, L95 (1989); N. Brummell, F. Cattaneo, J. Toomre, Science 269, 1370 (1995); Y.-C. Kim, P. A. Fox, S. Sofia, P. Demarque, Astrophys. J. 442, 422 (1995)].
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    • Early discussions of hydrogen fusion include C. F. von Weizsäcker, Phys. Z. 38, 176 (1937); G. Gamow, Phys. Rev. 53, 595 (1938); and H. A. Bethe, ibid. 55, 434 (1939). The details of the processes dominating energy generation in the sun, in the socalled pp chains, were elucidated by J. B. Oke [J. R. Astron. Soc. Can. 44, 135 (1950)]. Changes in the gravitational and internal energy, resulting from the fusion-induced changes of solar structure, also make a small contribution to the luminosity.
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    • Early discussions of hydrogen fusion include C. F. von Weizsäcker, Phys. Z. 38, 176 (1937); G. Gamow, Phys. Rev. 53, 595 (1938); and H. A. Bethe, ibid. 55, 434 (1939). The details of the processes dominating energy generation in the sun, in the socalled pp chains, were elucidated by J. B. Oke [J. R. Astron. Soc. Can. 44, 135 (1950)]. Changes in the gravitational and internal energy, resulting from the fusion-induced changes of solar structure, also make a small contribution to the luminosity.
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    • Early discussions of hydrogen fusion include C. F. von Weizsäcker, Phys. Z. 38, 176 (1937); G. Gamow, Phys. Rev. 53, 595 (1938); and H. A. Bethe, ibid. 55, 434 (1939). The details of the processes dominating energy generation in the sun, in the socalled pp chains, were elucidated by J. B. Oke [J. R. Astron. Soc. Can. 44, 135 (1950)]. Changes in the gravitational and internal energy, resulting from the fusion-induced changes of solar structure, also make a small contribution to the luminosity.
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    • Early discussions of hydrogen fusion include C. F. von Weizsäcker, Phys. Z. 38, 176 (1937); G. Gamow, Phys. Rev. 53, 595 (1938); and H. A. Bethe, ibid. 55, 434 (1939). The details of the processes dominating energy generation in the sun, in the socalled pp chains, were elucidated by J. B. Oke [J. R. Astron. Soc. Can. 44, 135 (1950)]. Changes in the gravitational and internal energy, resulting from the fusion-induced changes of solar structure, also make a small contribution to the luminosity.
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    • -1, respectively. For further details on the neutrino problem, see J. N. Bahcall, Neutrino Astrophysics (Cambridge Univ. Press, Cambridge, 1989); H. Dzitko, S. Turck-Chiėze, P. Delbourgo-Salvador, C. Lagrange, Astrophys. J. 447, 428 (1995); and (59).
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    • Although diffusion and settling were discussed by Eddington (5) and are unavoidable consequences of the normal assumptions of stellar modeling, their inclusion in detailed solar models is comparatively recent. See, for example, P. D. Noerdlinger, Astron. Astrophys. 57, 407 (1977); P. Demarque and D. B. Guenther, Advances in Helio- and Asteroseismology, J. Christensen-Dalsgaard and S. Frandsen, Eds. (IAU Symp. 123, Reidel, Dordrecht, 1988), p. 91; and (60); C. R. Proffitt and G. Michaud, Astrophys. J. 380, 238 (1991). The microscopic diffusion and settling rates were discussed by, for example, Michaud and Proffitt (61) and A. A. Thoul, J. N. Bahcall, and A. Loeb [Astrophys. J. 421, 828 (1994)].
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    • Although diffusion and settling were discussed by Eddington (5) and are unavoidable consequences of the normal assumptions of stellar modeling, their inclusion in detailed solar models is comparatively recent. See, for example, P. D. Noerdlinger, Astron. Astrophys. 57, 407 (1977); P. Demarque and D. B. Guenther, Advances in Helio- and Asteroseismology, J. Christensen-Dalsgaard and S. Frandsen, Eds. (IAU Symp. 123, Reidel, Dordrecht, 1988), p. 91; and (60); C. R. Proffitt and G. Michaud, Astrophys. J. 380, 238 (1991). The microscopic diffusion and settling rates were discussed by, for example, Michaud and Proffitt (61) and A. A. Thoul, J. N. Bahcall, and A. Loeb [Astrophys. J. 421, 828 (1994)].
    • (1988) Advances in Helio- and Asteroseismology , pp. 91
    • Demarque, P.1    Guenther, D.B.2
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    • 0041881169 scopus 로고
    • Although diffusion and settling were discussed by Eddington (5) and are unavoidable consequences of the normal assumptions of stellar modeling, their inclusion in detailed solar models is comparatively recent. See, for example, P. D. Noerdlinger, Astron. Astrophys. 57, 407 (1977); P. Demarque and D. B. Guenther, Advances in Helio- and Asteroseismology, J. Christensen-Dalsgaard and S. Frandsen, Eds. (IAU Symp. 123, Reidel, Dordrecht, 1988), p. 91; and (60); C. R. Proffitt and G. Michaud, Astrophys. J. 380, 238 (1991). The microscopic diffusion and settling rates were discussed by, for example, Michaud and Proffitt (61) and A. A. Thoul, J. N. Bahcall, and A. Loeb [Astrophys. J. 421, 828 (1994)].
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    • Although diffusion and settling were discussed by Eddington (5) and are unavoidable consequences of the normal assumptions of stellar modeling, their inclusion in detailed solar models is comparatively recent. See, for example, P. D. Noerdlinger, Astron. Astrophys. 57, 407 (1977); P. Demarque and D. B. Guenther, Advances in Helio- and Asteroseismology, J. Christensen-Dalsgaard and S. Frandsen, Eds. (IAU Symp. 123, Reidel, Dordrecht, 1988), p. 91; and (60); C. R. Proffitt and G. Michaud, Astrophys. J. 380, 238 (1991). The microscopic diffusion and settling rates were discussed by, for example, Michaud and Proffitt (61) and A. A. Thoul, J. N. Bahcall, and A. Loeb [Astrophys. J. 421, 828 (1994)].
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    • The mass of the sun is known from planetary motion, and the radius of the visible surface can be measured directly. The solar luminosity is inferred from spacebased irradiance measurements (R. C. Wilson and H. S. Hudson, Nature 332, 810 (1988)], assuming isotropic radiation and averaging over the solar-cycle variation of about 0.1 % [for stellar evidence, see S. Baliunas and R. Jastrow, Nature 348, 520 (1990)].
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    • The abundances of elements other than helium can in general be determined with considerable precision [E. Anders and N. Grevesse, Geochim. Cosmochim. Acta 53, 197 (1989); N. Grevesse and A. Noels, in Origin and Evolution of the Elements, N. Prantzos, E. Vangioni, M. Cassé, Eds. (Cambridge Univ. Press, Cambridge, 1993), p. 15). Although helium was first detected in the solar spectrum, the formation of the helium lines is so complex that observation gives no precise information about its abundance.
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    • Rotationally induced mixing was considered by B. Cnaboyer, P. Demarque, D. B. Guenther, and M. H. Pinsonneault [Astrophys. J. 446, 435 (1995)] and by O. Richard, S. Vauclair, C. Charbonnel, and W. A. Dziembowski [Astron. Astrophys., in press]. Simple models of penetration beneath the convection zone predict a region of nearly adiabatic stratification, followed by a sharp transition to radiative transport [J. H. M. M. Schmitt, R. Rosner, H. U. Bohn, Astrophys. J. 282, 316 (1984); J.-P. Zahn, Astron. Astrophys. 252, 179 (1991)]. The extent of penetration in such simple models has been constrained to a small fraction of a pressure scale height by helioseismic analyses [S. Basu, H. M. Antia, D. Narasimha, Mon. Not. R. Astron. Soc. 267, 209 (1994), M. J. P. F. G. Monteiro, J. Christensen-Dalsgaard, M. J. Thompson, Astron. Astrophys. 283, 247 (1994); I. W. Roxburgh and S. V. Vorontsov, Mon. Not. R. Astron. Soc. 268, 880 (1994)]. Beyond the region of penetration, which is certainly fully mixed, additional mixing might be caused by gravity waves induced by the penetration.
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    • Rotationally induced mixing was considered by B. Cnaboyer, P. Demarque, D. B. Guenther, and M. H. Pinsonneault [Astrophys. J. 446, 435 (1995)] and by O. Richard, S. Vauclair, C. Charbonnel, and W. A. Dziembowski [Astron. Astrophys., in press]. Simple models of penetration beneath the convection zone predict a region of nearly adiabatic stratification, followed by a sharp transition to radiative transport [J. H. M. M. Schmitt, R. Rosner, H. U. Bohn, Astrophys. J. 282, 316 (1984); J.-P. Zahn, Astron. Astrophys. 252, 179 (1991)]. The extent of penetration in such simple models has been constrained to a small fraction of a pressure scale height by helioseismic analyses [S. Basu, H. M. Antia, D. Narasimha, Mon. Not. R. Astron. Soc. 267, 209 (1994), M. J. P. F. G. Monteiro, J. Christensen-Dalsgaard, M. J. Thompson, Astron. Astrophys. 283, 247 (1994); I. W. Roxburgh and S. V. Vorontsov, Mon. Not. R. Astron. Soc. 268, 880 (1994)]. Beyond the region of penetration, which is certainly fully mixed, additional mixing might be caused by gravity waves induced by the penetration.
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    • Rotationally induced mixing was considered by B. Cnaboyer, P. Demarque, D. B. Guenther, and M. H. Pinsonneault [Astrophys. J. 446, 435 (1995)] and by O. Richard, S. Vauclair, C. Charbonnel, and W. A. Dziembowski [Astron. Astrophys., in press]. Simple models of penetration beneath the convection zone predict a region of nearly adiabatic stratification, followed by a sharp transition to radiative transport [J. H. M. M. Schmitt, R. Rosner, H. U. Bohn, Astrophys. J. 282, 316 (1984); J.-P. Zahn, Astron. Astrophys. 252, 179 (1991)]. The extent of penetration in such simple models has been constrained to a small fraction of a pressure scale height by helioseismic analyses [S. Basu, H. M. Antia, D. Narasimha, Mon. Not. R. Astron. Soc. 267, 209 (1994), M. J. P. F. G. Monteiro, J. Christensen-Dalsgaard, M. J. Thompson, Astron. Astrophys. 283, 247 (1994); I. W. Roxburgh and S. V. Vorontsov, Mon. Not. R. Astron. Soc. 268, 880 (1994)]. Beyond the region of penetration, which is certainly fully mixed, additional mixing might be caused by gravity waves induced by the penetration.
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    • Rotationally induced mixing was considered by B. Cnaboyer, P. Demarque, D. B. Guenther, and M. H. Pinsonneault [Astrophys. J. 446, 435 (1995)] and by O. Richard, S. Vauclair, C. Charbonnel, and W. A. Dziembowski [Astron. Astrophys., in press]. Simple models of penetration beneath the convection zone predict a region of nearly adiabatic stratification, followed by a sharp transition to radiative transport [J. H. M. M. Schmitt, R. Rosner, H. U. Bohn, Astrophys. J. 282, 316 (1984); J.-P. Zahn, Astron. Astrophys. 252, 179 (1991)]. The extent of penetration in such simple models has been constrained to a small fraction of a pressure scale height by helioseismic analyses [S. Basu, H. M. Antia, D. Narasimha, Mon. Not. R. Astron. Soc. 267, 209 (1994), M. J. P. F. G. Monteiro, J. Christensen-Dalsgaard, M. J. Thompson, Astron. Astrophys. 283, 247 (1994); I. W. Roxburgh and S. V. Vorontsov, Mon. Not. R. Astron. Soc. 268, 880 (1994)]. Beyond the region of penetration, which is certainly fully mixed, additional mixing might be caused by gravity waves induced by the penetration.
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    • note
    • We thank R. Trampedach for assistance with the graphics. The work reported here was supported in part by the Danish National Research Foundation through the establishment of the Theoretical Astrophysics Center and in part by grant AST-9315112 from National Science Foundation (NSF). The GONG is managed by the National Solar Observatory, a division of the National Optical Astronomy Observatories, operated by Association of Universities for Research in Astronomy under a cooperative agreement with NSF. The data were acquired by instruments operated by the Big Bear Solar Observatory, High Altitude Observatory, Learmonth Solar Observatory, Udaipur Solar Observatory, Instituto de Astrofisica de Canarias, and Cerro Toblo Interamerican Observatory.


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