CONVECTION AND DIFFERENTIAL ROTATION IN F-TYPE STARS

被引:50
作者
Augustson, Kyle C. [1 ,2 ]
Brown, Benjamin P. [3 ,4 ]
Brun, Allan Sacha [5 ,6 ]
Miesch, Mark S. [7 ]
Toomre, Juri [1 ,2 ]
机构
[1] Univ Colorado, JILA, Boulder, CO 80309 USA
[2] Univ Colorado, Dept Astrophys & Planetary Sci, Boulder, CO 80309 USA
[3] Univ Wisconsin, Dept Astron, Madison, WI 53706 USA
[4] Univ Wisconsin, Ctr Magnet Self Org CMSO Lab & Astrophys Plasmas, Madison, WI 53706 USA
[5] Univ Paris 07, UMR AIM, CEA, CNRS, F-91191 Gif Sur Yvette, France
[6] CEA Saclay, DSM IRFU SAp, F-91191 Gif Sur Yvette, France
[7] High Altitude Observ, Boulder, CO 80301 USA
基金
美国国家科学基金会;
关键词
convection; hydrodynamics; stars: interiors; stars: rotation; stars: solar-type; TRANSPORT DYNAMO MODELS; COMPRESSIBLE CONVECTION; SOLAR CONVECTION; TURBULENT CONVECTION; SPHERICAL-SHELLS; NUMERICAL SIMULATIONS; SUNS INTERIOR; EVOLUTION; TACHOCLINE; FLOWS;
D O I
10.1088/0004-637X/756/2/169
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Differential rotation is a common feature of main-sequence spectral F-type stars. In seeking to make contact with observations and to provide a self-consistent picture of how differential rotation is achieved in the interiors of these stars, we use the three-dimensional anelastic spherical harmonic (ASH) code to simulate global-scale turbulent flows in 1.2 and 1.3 M-circle dot F-type stars at varying rotation rates. The simulations are carried out in spherical shells that encompass most of the convection zone and a portion of the stably stratified radiative zone below it, allowing us to explore the effects of overshooting convection. We examine the scaling of the mean flows and thermal state with rotation rate and mass and link these scalings to fundamental parameters of the simulations. Indeed, we find that the differential rotation becomes much stronger with more rapid rotation and larger mass, scaling as Delta Omega proportional to M-3.9 Omega(0.6)(0). Accompanying the growing differential rotation is a significant latitudinal temperature contrast, with amplitudes of 1000 K or higher in the most rapidly rotating cases. This contrast in turn scales with mass and rotation rate as Delta T proportional to M-6.4 Omega(1.6)(0). On the other hand, the meridional circulations become much weaker with more rapid rotation and with higher mass, with their kinetic energy decreasing as KEMC proportional to M-1.2 Omega(-0.8)(0). Additionally, three of our simulations exhibit a global-scale shear instability within their stable regions that persists for the duration of the simulations. The flow structures associated with the instabilities have a direct coupling to and impact on the flows within the convection zone.
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页数:23
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