首页> 外文期刊>The Astrophysical journal >HELIOSEISMIC OBSERVATION OF THE STRUCTURE AND DYNAMICS OF A ROTATING SUNSPOT BENEATH THE SOLAR SURFACE
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HELIOSEISMIC OBSERVATION OF THE STRUCTURE AND DYNAMICS OF A ROTATING SUNSPOT BENEATH THE SOLAR SURFACE

机译:太阳表面下旋转太阳黑子的结构和动力学的减震观测

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摘要

Time-distance helioseismology is applied to study the subphotospheric structures and dynamics of an unusually fast-rotating sunspot observed by the Michelson Doppler Imager on board SOHO in 2000 August. The subsurface sound speed structures and velocity fields are obtained for the sunspot region at different depths from 0 to 12 Mm. By comparing the subsurface sound speed variations with the surface magnetic field, we find evidence for structural twists beneath the visible surface of this active region, which may indicate that magnetic twists often seen at the photosphere also exist beneath the photosphere. We also report on the observation of subsurface horizontal vortical flows that extend to a depth of 5 Mm around this rotating sun-spot and present evidence that opposite vortical flows may exist below 9 Mm. It is suggested that the vortical flows around this active region may build up a significant amount of magnetic helicity and energy to power solar eruptions. Monte Carlo simulation has been performed to estimate the error propagation, and in addition the sunspot umbra is masked to test the reliability of our inversion results. On the basis of the three-dimensional velocity fields obtained from the time-distance helioseismology inversions, we estimate the subsurface kinetic helicity at different depths for the first time and conclude that it is comparable to the current helicity estimated from vector magnetograms.
机译:2000年8月,由迈克尔逊·多普勒成像仪在SOHO上观测到的时空日变地震学被用于研究一个异常快速旋转的太阳黑子的亚光圈结构和动力学。在0到12 Mm的不同深度获得了黑子区域的地下声速结构和速度场。通过将地下声速变化与表面磁场进行比较,我们发现了在该有源区域的可见表面下方存在结构扭曲的证据,这可能表明通常在光层看到的磁扭曲也存在于光层之下。我们还报告了围绕该旋转太阳黑点延伸至5 Mm深度的地下水平涡流的观察结果,并提供了证据表明在9 Mm以下可能存在相反的涡流。建议在该活动区域周围的涡流可能会形成大量的磁螺旋和能量来为太阳爆发提供动力。已经进行了蒙特卡洛模拟以估计误差传播,此外,对黑子本影进行了掩盖以测试我们反演结果的可靠性。根据从时距螺旋地震学反演获得的三维速度场,我们首次估计了不同深度的地下动力螺旋度,并得出结论,其与矢量磁图估计的当前螺旋度具有可比性。

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