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The Department of Ecology estimates the addition of nearly 500 annual trips in and out of the port, on top of the approximately 2,700 current crossings through northern Puget Sound.
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Fast magnetic field polarity changes detected in the quiet magnetotail by a spacecraft are usually attributed to thin cross-tail current sheet crossings.
A dipole tilt and/or current sheet crossings are unlikely causes for such periodic perturbations.
We applied a superposed epoch analysis to simple, monotonous current sheet crossings and obtained a statistical profile of the current sheet.
The four bottom panels (k n) show the average ion flows perpendicular to the magnetic field (green) and electric field (dark blue) during the four current sheet crossings (i iv).
The current zero-crossing point is generated by an oscillating current.
Before the current zero-crossing point, the fault resistance increases sharply, resulting in a very small current value (Zones 1 and 3 in Fig. 7).
The fault analysis method and the fast DC circuit breaker design method based on the natural current zero-crossing point can apply to different voltages.
Thus, it can be realized through detecting sudden changes in the voltage to determine the fault time and the current zero-crossing time.
The given VSC-HVDC model was simulated off-line and the relationship between the recorded data suddenly changed the voltage and current zero-crossing time.
Then, a fast solid state DC circuit breaker design method based on the natural current zero-crossing point at an inverter station is proposed.
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