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On the generation, propagation and radiation of magneto-acoustic-gravity waves with application to stars

机译:关于磁声重力波的产生,传播和辐射及其在恒星上的应用

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The propagation, generation and radiation of magneto-acoustic-gravity (MAG) waves are modelled using the approach of a "wave analogy" (Campos 1987) analogous to the original "acoustic analogy" (Lighthill 1952), viz.: (i) the starting point is the general equations of magnetohydrodynamics (MHD) describing a viscous electrically conducting fluid in the presence of magnetic and gravity fields; (ii) a steady inhomogeneous mean state is considered, i.e. an atmosphere under non-uniform gravity and external magnetic field; (iii) the linear non-dissipative perturbation terms are eliminated for the velocity perturbation, leading to the magneto-acoustic-gravity wave operator, which combines sound, Alfvn and internal waves and their interactions; (iv) the non-linear and dissipative terms are retained to model the sources of MAG waves, which consist of an hydronamic tensor (Lighthill 1952), an analogous hydromagnetic tensor (Campos 1977), and a "new" hydrogravity tensor. For MAG wave propagation within an atmospheric scale height, the dispersion matrix is used to calculate the radiation field, leading to an estimate of the wave energy flux in the far field. The latter is calculated for the solar chromosphere, and is found to be comparable to the solar radiative losses, suggesting that hydromagnetic turbulence and ionized inhomogeneities are the sources of MAG waves which transport a substantial energy flux through the atmosphere of the sun. A second application is made to estimate the magnitude of magnetic non-degenerate stars based on the assumption that their luminosity is due to energy transport by MAG waves, whose sources are predominantly hydromagnetic; this leads to a scaling law between stellar magnitude and magnetic field strength, which may be a reasonable alternative to the Hertzsprung-Russell diagram for magnetic non-degenerate stars. This suggests that hydromagnetic sources of MAG waves dominate the energy transport in stellar atmospheres for r.m.s. magnetic field strengths of the order of 150 G or more.
机译:磁声重力波(MAG)的传播,产生和辐射是通过类似于原始“声波模拟”(Lighthill 1952)的“波模拟”(Campos 1987)的方法建模的,即:(i)起点是磁流体动力学(MHD)的一般方程,描述了在磁场和重力场存在下的粘性导电流体。 (ii)考虑到稳定的不均匀平均状态,即重力和外部磁场不均匀的气氛; (iii)消除了线性非耗散扰动项以进行速度扰动,从而产生了磁声重力波算子,该算子将声音,Alfvn和内部波及其相互作用结合在一起; (iv)保留非线性项和耗散项以模拟MAG波的来源,其中包括一个水文张量(Lighthill 1952),类似的水磁张量(Campos 1977)和一个“新的”水重力张量。对于在大气尺度高度内的MAG波传播,使用色散矩阵来计算辐射场,从而估算远场中的波能通量。后者是针对太阳色球层计算得出的,并且与太阳辐射损失相当,这表明水磁湍流和电离不均匀性是MAG波的来源,它们通过太阳大气传输大量的能量通量。第二个应用是基于以下假设来估计未变星的磁星的亮度,即它们的光度是由于MAG波的能量传输所致,而MAG波的来源主要是水磁。这导致了恒星大小和磁场强度之间的比例定律,这对于非简并磁星可能是Hertzsprung-Russell图的合理替代。这表明MAG波的水磁源主导着恒星大气在r.m.s的能量传输。磁场强度约为150 G或更高。

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