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Evolution of Relative Magnetic Helicity: Method of Computation and Its Application to a Simulated Solar Corona above an Active Region

机译:相对磁螺旋的演化:计算方法及其在有源区上方模拟太阳日冕中的应用

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For a better understanding of solar magnetic field evolution it is appropriate to evaluate the magnetic helicity based on observations and to compare it with numerical simulation results. We have developed a method for calculating the vector potential of a magnetic field given in a finite volume; the method requires the magnetic flux to be balanced on all the side boundaries of the considered volume. Our method uses a fast Laplace/Poisson solver to obtain the vector potentials for a given magnetic field and for the corresponding potential (current-free) field. This allows an efficient calculation of the relative magnetic helicity in a finite 3D volume. We tested our approach on a theoretical model (Low and Lou, Astrophys. J. 352, 343, 1990) and also applied our method to the magnetic field above active region NOAA 8210 obtained by a photospheric-data-driven MHD model. We found that the amount of accumulated relative magnetic helicity coincides well with the relative helicity inflow through the boundaries in the ideal and non-ideal cases. The temporal evolution of relative magnetic helicity is consistent with that of magnetic energy. The maximum value of normalized helicity, Hm/Φ2=0. 0298, is reached just before a drastic energy release by magnetic reconnection. This value is close to the corresponding value inferred from the formula that connects the magnetic flux and the accumulated magnetic helicity based on the observations of solar active regions.
机译:为了更好地了解太阳磁场的演化,应该根据观测结果评估磁螺旋度并将其与数值模拟结果进行比较。我们已经开发出一种用于计算有限体积内的磁场矢量势的方法;该方法要求在所考虑体积的所有侧面边界上平衡磁通量。我们的方法使用快速Laplace / Poisson求解器来获得给定磁场和相应势场(无电流)的矢量势。这允许在有限的3D体积中有效地计算相对磁螺旋度。我们在理论模型上测试了我们的方法(Low and Lou,Astrophys。J. 352,343,1990),还将我们的方法应用于由光球数据驱动的MHD模型获得的活动区域NOAA 8210上方的磁场。我们发现,在理想和非理想情况下,相对磁螺旋的累积量与通过边界的相对螺旋流入量非常吻合。相对磁螺旋的时间演化与磁能的一致。标准化螺旋度的最大值Hm /Φ2= 0。通过磁重新连接释放巨大能量之前,达到0298。该值接近根据太阳活动区域的观察结果从连接磁通量和累积的磁螺旋度的公式得出的对应值。

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