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Associating ground magnetometer observations with current or voltage generators

机译:将地磁测量仪观测与电流或电压发生器相关联

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摘要

A circuit analogy for magnetosphere-ionosphere current systems has two extremes for driversof ionospheric currents: ionospheric elec tric fields/voltages constant while current/conductivity vary—the“voltage generator”—and current constant while electric field/conductivity vary—the “current generator.”Statistical studies of ground magnetometer observations associated with dayside Transient High LatitudeCurrent Systems (THLCS) driven by similar mechanisms find contradictory results using this paradigm:some studies associate THLCS with voltage generators, others with current generators. We argue that mostof this contradiction arises from two assumptions used to interpret ground magnetometer observations:(1) measurements made at fixed position relative to the THLCS field-aligned current and (2) negligibleauroral precipitation contributions to ionospheric conductivity. We use observations and simulations toillustrate how these two assumptions substantially alter expectations for magnetic perturbations associatedwith either a current or a voltage generator. Our results demonstrate that before interpreting groundmagnetometer observations of THLCS in the context of current/voltage generators, the location of a groundmagnetometer station relative to the THLCS field-aligned current and the location of any auroral zoneconductivity enhancements need to be taken into account.
机译:磁层-电离层电流系统的电路模拟对于电离层电流的驱动器有两个极端:电离层电场/电压恒定,而电流/电导率变化(“电压发生器”),而电常数/电场/电导率变化时的电流常数(“电流发生器”)使用类似机制驱动的与日间暂态高纬度电流系统(THLCS)相关的地面磁力计观测数据的统计研究,发现使用这种范例的结果相互矛盾:一些研究将THLCS与电压发生器相关联,另一些研究与电流发生器相关联。我们认为,大多数矛盾是由用于解释地面磁力计观测的两个假设引起的:(1)在相对于THLCS场对准电流的固定位置进行的测量,以及(2)极小的耳廓降水对电离层电导率的贡献。我们使用观察和模拟来说明这两个假设如何实质上改变对与电流或电压发生器相关的磁扰动的期望。我们的结果表明,在解释电流/电压发生器中THLCS的地磁仪观测值之前,必须考虑地磁仪站相对于THLCS场对准电流的位置以及任何极光区电导率增强的位置。

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