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The Dynamic Evolution of Twisted Magnetic Flux Tubes in a Three-dimensional Convecting Flow. I. Uniformly Buoyant Horizontal Tubes

机译:三维对流中扭曲磁通量管的动态演化。 I.均匀浮力的水平管

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We present three-dimensional numerical simulations of the dynamic evolution of uniformly buoyant, twisted horizontal magnetic flux tubes in a three-dimensional stratified convective velocity field. Our calculations are relevant to understanding how stratified convection in the deep solar convection zone may affect the rise and the structure of buoyant flux tubes that are responsible for the emergence of solar active regions. We find that in order for the magnetic buoyancy force of the tube to dominate the hydrodynamic force due to the convective downflows, the field strength B of the flux tube needs to be greater than (Hp/a)1/2Beq ~ 3Beq, where Hp is the pressure scale height, a is the tube radius, and Beq is the field strength in equipartition with the kinetic energy density of the strong downdrafts. For tubes of equipartition field strength (B = Beq), the dynamic evolution depends sensitively on the local condition of the convective flow. Sections of the tube in the paths of strong downdrafts are pinned down to the bottom despite their buoyancy, while the rise speed of sections within upflow regions is significantly boosted; Ω-shaped emerging tubes can form between downdrafts. Although flux tubes with B = Beq are found to be severely distorted by convection, the degree of distortion obtained from our simulations is not severe enough to clearly rule out the Ω-tubes that are able to emerge between downdrafts as possible progenitors of solar active regions. As the initial field strength of the tube becomes higher than the critical value of ~(Hp/a)1/2Beq given above, the dynamic evolution converges toward the results of previous simulations of the buoyant rise of magnetic flux tubes in a static, adiabatically stratified model solar convection zone. Tubes with 10 times the equipartition field strength are found to rise unimpeded by the downdrafts and are not significantly distorted by the three-dimensional convective flow.
机译:我们在三维分层对流速度场中提供均匀浮力,扭曲的水平磁通量管动态演化的三维数值模拟。我们的计算与理解深层太阳对流层中的分层对流如何影响负责太阳活动区域出现的浮力式通量管的结构和结构有关。我们发现,为了使管的磁性浮力在对流向下流动的作用下支配流体动力,通量管的场强B必须大于(Hp / a)1 / 2Beq〜3Beq,其中Hp是压力标尺高度,a是管半径,Beq是与强下降气流的动能密度相等的场强。对于等分场强(B = Beq)的管,动态演化敏感地取决于对流的局部条件。尽管有浮力,但在强力下降气流路径中的管段被固定在底部,而上流区内的管段的上升速度明显提高。下降流之间会形成Ω形新兴管。尽管发现B = Beq的通量管因对流而严重变形,但从我们的模拟中获得的变形程度还不够严重,无法清楚地排除能够在下降气流之间出现的Ω管作为太阳活动区域的祖先。随着管的初始场强变得高于上述给定的〜(Hp / a)1 / 2Beq的临界值,动态演化趋向于先前的静态,绝热状态下磁通管浮力上升的模拟结果。分层模型的太阳对流区。已发现等分场强为10倍的管不受下流阻力的影响而上升,并且不受三维对流的影响而明显变形。

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