Detectability of large-scale flows in global helioseismic data: A numerical experiment
Detectability of large-scale flows in global helioseismic data: A numerical experiment
复制标题
全球日震数据中大尺度流的可检测性:数值实验
DOI:
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发表时间:
2002
期刊:
影响因子:
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通讯作者:
R. Komm
中科院分区:
文献类型:
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作者:
M. Roth;R. Howe;R. Komm
Convective motions affect the solar p-modes by shifting their frequencies. In comparison to the frequency splitting caused by the differential rotation, this is only a small additional effect. As the spatial resolution of the inversions for the differ- ential rotation becomes better, it is important to know how these additional frequency shifts modify the splitting coefficients and how these two effects might be disentangled. Therefore we carry out a numerical experiment. We use quasi-degenerate pertur- bation theory to create frequencies of p-modes that are affected by differential rotation and by large-scale flows. The simulated frequency sets are analyzed and inverted for differential rotation. We use changes in the (l ,ν ) coverage, the multiplets, and the inversion results as diagnostics to draw conclusions about the detectability of large-scale flows in global helioseismic data. The result is a detectability limit of the order of 10ms −1 for large-scale flows in the convection zone. A sectoral poloidal flow with greater amplitude will lead to a noticeable distortion of the rotation rate, while a zonal poloidal flow with greater amplitude will lead to distorted even-a coefficients and disrupted multiplets. In this study, we search for large-scale, long-lived struc- tures in the convection zone by using global helioseismol- ogy results combined with quasi-degenerate perturbation the- ory and numerical simulations. We concentrate on changes in the (l ,ν ) coverage, the multiplets, and the inversion results and derive detectability limits for the velocity of large-scale structures. The motivation for this study is two-fold. On the one hand, the internal structure of the Sun has been determined with in- creasing accuracy within the last few years. Especially with the availability of high-quality helioseismic data the properties of the differential rotation and its depth dependence have been studied in great detail by inverting oscillation data. Because of the improving resolution of the solar interior, it is necessary to know about smaller effects of physical processes in the sun on the solar oscillations and their influences on the inversion results.