“…For obtaining a harmonic source location, the emitted harmonic magnitude can be used to determine harmonic sources using active models such as the Norton model at harmonic frequencies [23], as a traditional method in the frequency domain; also, the time-varying equivalent impedance parameters can be used to determine harmonic sources, as a method in the time domain. The equivalent impedance waveforms in the time domain are obtained by sequentially solving (2). In fundamental cycles of grid frequency, equivalent impedance waveforms of linear loads generally remain stable, while severe fluctuations in equivalent impedance waveforms of nonlinear loads are easily observed [6], [18]- [21].…”