Linear Phase Terms

The reason $e^{-j \omega_k \Delta}$ is called a linear phase term is that its phase is a linear function of frequency:

$$\angle e^{-j \omega_k \Delta} = - \Delta \cdot \omega_k$$

Thus, the slope of the phase, viewed as a linear function of radian-frequency $\omega_k$ , is $-\Delta$ . In general, the time delay in samples equals minus the slope of the linear phase term. If we express the original spectrum in polar form as

$$X(k) = G(k) e^{j\Theta(k)},$$

where $G$ and $\Theta$ are the magnitude and phase of $X$ , respectively (both real), we can see that a linear phase term only modifies the spectral phase $\Theta(k)$ :

$$e^{-j \omega_k \Delta} X(k) \isdef e^{-j \omega_k \Delta} G(k) e^{j\Theta(k)} = G(k) e^{j[\Theta(k)-\omega_k\Delta]}$$

where $\omega_k\isdeftext 2\pi k/N$ . A positive time delay (waveform shift to the right) adds a negatively sloped linear phase to the original spectral phase. A negative time delay (waveform shift to the left) adds a positively sloped linear phase to the original spectral phase. If we seem to be belaboring this relationship, it is because it is one of the most useful in practice.