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A comparison of the probability distribution of observed substorm magnitude with that predicted by a minimal substorm model

机译:观测到的亚暴幅度与最小亚暴模型预测的概率分布的比较

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摘要

We compare the probability distributions of substorm magnetic bay magnitudes from observations and a minimal substorm model. The observed distribution was derived previously and independently using the IL index from the IMAGE magnetometer network. The model distribution is derived from a synthetic AL index time series created using real solar wind data and a minimal substorm model, which was previously shown to reproduce observed substorm waiting times. There are two free parameters in the model which scale the contributions to AL from the directly-driven DP2 electrojet and loading-unloading DP1 electrojet, respectively. In a limited region of the 2-D parameter space of the model, the probability distribution of modelled substorm bay magnitudes is not significantly different to the observed distribution. The ranges of the two parameters giving acceptable (95% confidence level) agreement are consistent with expectations using results from other studies. The approximately linear relationship between the two free parameters over these ranges implies that the substorm magnitude simply scales linearly with the solar wind power input at the time of substorm onset.
机译:我们从观测资料和最小亚暴风模型中比较了亚暴磁海湾震级的概率分布。所观察到的分布是事先从IMAGE磁力计网络中使用IL指数独立得出的。该模型分布来自使用实际太阳风数据和最小亚风暴模型创建的合成AL指数时间序列,该模型先前已显示出可再现观测到的亚风暴等待时间。该模型中有两个自由参数,分别用于衡量直接驱动的DP2电喷和装卸DP1电喷对AL的贡献。在模型的二维参数空间的有限区域中,模拟的亚风暴海湾震级的概率分布与观测到的分布没有显着差异。给出可接受(95%置信度)一致性的两个参数的范围与使用其他研究结果得出的预期一致。在这些范围内,两个自由参数之间的近似线性关系意味着,亚暴发生时,亚暴幅度仅与输入的太阳风能成线性比例关系。

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