“…In both time and frequency domains, ground motions are typical non-stationary signals. The non-stationary property has been widely studied, 1 methods to generate non-stationary ground motions, 2,3 especially non-stationary ground motion in two orthogonal horizontal directions, 4,5 have gained increasing attention recently. The non-stationary frequency content is harder to describe than amplitude content; therefore, some methods are put forward, such as Fourier transform, physical spectrum, 6 Hilbert transform and Hilbert-Huang transform, 7,8 wavelet transform, 9,10 zero-crossing rate, 11 and univariate phase spectrum model.…”