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Surface electric fields and geomagnetically inducedudcurrents in the Scottish Power grid duringudthe 30 October 2003 geomagnetic storm

机译:表面电场和地磁诱导 ud ud期间苏格兰电网的电流2003年10月30日的地磁风暴

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摘要

A surface electric field model is used to estimate the UK surface E field during the 30 October 2003udsevere geomagnetic storm. This model is coupled with a power grid model to determine the flow ofudgeomagnetically induced currents (GIC) through the Scottish part of the UK grid. Model data areudcompared with GIC measurements at four sites in the power network. During this storm, measured andudmodeled GIC levels exceeded 40 A, and the surface electric field reached 5 V/km at sites in the UnitedudKingdom (compared with quiet-time levels of less than 0.1 V/km). The electric field and grid models nowudform part of a GIC monitoring, analysis, and warning software package with Web interface, developed foruduse by the grid operator. This package also contains a daily geomagnetic activity forecast service, a solarudwind shock detector for geomagnetic storm warning, and a near-real-time geomagnetic data stream forudstorm monitoring.
机译:在2003年10月30日强烈的地磁风暴中,地表电场模型用于估算英国的地表E场。该模型与电网模型耦合,以确定通过英国电网苏格兰部分的磁感应电流(GIC)的流动。模型数据与电网中四个站点的GIC测量结果进行了比较。在这场暴风雨期间,测量和模拟的GIC电平超过40 A,联合王国站点的地面电场达到5 V / km(相比之下,安静时间电平小于0.1 V / km)。电场和网格模型现在已构成具有Web界面的GIC监视,分析和警告软件包的一部分,该软件包是由网格操作员开发的。该软件包还包含每日地磁活动预测服务,用于地磁风暴预警的日/风冲击探测器以及用于暴雨监测的近实时地磁数据流。

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