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Improved Euler potential method for three-dimensional magnetospheric equilibrium

机译:改进的欧拉方法的潜力三维磁性层的平衡

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A new Euler potential method is presented for computing 3-D magnetospheric equilibria with prescribed plasma pressure, that significantly improves on a previous flux coordinate approach. In the new approach, the Euler potential α is no longer necessarily the magnetic flux, but can be specified much more freely, allowing equilibrium calculations in much more extended magnetospheric domains. With an empirical plasma pressure model as input and the T96 empirical magnetic field for boundary conditions, the new method is applied to compute a force balanced quiet time magnetospheric state extending to 30 R E in the magnetotail. While the force-balanced results for the magnetic field are not too different from T96 on the midnight axis, a very large discrepancy is found between field aligned currents (FACs) in the force balanced state and those computed from the empirical field and pressure using Vasyliunas equation; this shows that explicitly computed force balance is required for deriving FACs from plasma pressure and magnetic field by way of Vasyliunas equation.
机译:一个新的欧拉的潜在方法计算三维磁性层的平衡规定的等离子体压力明显在先前的通量提高协调方法。在新方法中,欧拉潜在α是否定的长一定是磁通,但可以指定更多的自由,允许平衡计算磁性层的扩展得多域。作为输入和T96实证磁场边界条件,应用新方法计算一个力平衡的安静的时间延长到30 R E的磁性层的状态磁尾。磁场不太与T96不同在午夜的轴,一个非常大的差异发现场电流(流式细胞仪)保持一致从力平衡状态和计算使用Vasyliunas实证领域和压力方程;从力平衡推导需要流式细胞仪等离子体压力和磁场的方式Vasyliunas方程。

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