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In physics and mathematics, the phase of a periodic function ${\displaystyle F}$ of some variable ${\displaystyle t}$ is the relative value of that variable within the span of each full period.

The phase is typically expressed as an angle ${\displaystyle \varphi (t)}$, in such a scale that it varies by one full turn as the variable ${\displaystyle t}$ goes through each period (and ${\displaystyle F(t)}$ goes through each complete cycle). Thus, if the phase is expressed in degrees, it will increase by 360° as ${\displaystyle t}$ increases by one period. If it is expressed in radians, the same increase in ${\displaystyle t}$ will increase the phase by ${\displaystyle 2\pi }$.

This convention is especially appropriate for a sinusoidal function, since its value at any argument ${\displaystyle t}$ then can be expressed as the sine or cosine of the phase ${\displaystyle \varphi (t)}$, multiplied by some factor (the amplitude of the sinusoid).

Usually, whole turns are ignored when expressing the phase; so that ${\displaystyle \varphi (t)}$ is also a periodic function, with the same period as ${\displaystyle F}$, that repeatedly scans the same range of angles as ${\displaystyle t}$ goes through each period. In degrees, the range is usually from 0° to 360°, or from −180° to +180°. In radians, it is usually from 0 to ${\displaystyle 2\pi }$, or from ${\displaystyle -\pi }$ to ${\displaystyle +\pi }$. Then, ${\displaystyle F}$ is said to be "at the same phase" at two argument values ${\displaystyle t_{1}}$ and ${\displaystyle t_{2}}$ (that is, ${\displaystyle \varphi (t_{1})=\varphi (t_{2})}$) if the difference between them is a whole number of periods.

In any case, the numeric value of the phase ${\displaystyle \varphi (t)}$ depends on the arbitrary choice of the start of each period of the argument variable ${\displaystyle t}$, and on the interval of angles that each period is to be mapped to.

The term "phase" is also used to describe a shift that is applied to the argument of a periodic function, when such a shift is expressed as a fraction of the period and converted to an angle. Such a shift could correspondint to a change of origin for the argument variable. This concept is more properly called phase shift, phase offset, or initial phase.

Phase shift

Phase shift is any change that occurs in the phase of one quantity, or in the phase difference between two or more quantities.

This symbol: ${\displaystyle \varphi }$ is sometimes referred to as a phase shift or phase offset because it represents a "shift" from zero phase.

For infinitely long sinusoids, a change in ${\displaystyle \varphi }$ is the same as a shift in time, such as a time delay. If ${\displaystyle \textstyle x(t)}$ is delayed (time-shifted) by ${\displaystyle \textstyle {\frac {1}{4}}}$ of its cycle, it becomes:

${\displaystyle {\begin{aligned}x\left(t-{\tfrac {1}{4}}T\right)&=A\cdot \cos \left(2\pi f\left(t-{\tfrac {1}{4}}T\right)+\varphi \right)\\&=A\cdot \cos \left(2\pi ft-{\tfrac {\pi }{2}}+\varphi \right)\end{aligned}}}$

whose "phase" is now ${\displaystyle \textstyle \varphi -{\frac {\pi }{2}}}$. It has been shifted by ${\displaystyle \textstyle {\frac {\pi }{2}}}$ radians (the variable ${\displaystyle A}$ here just represents the amplitude of the wave).

Phase difference

Phase difference is the difference, expressed in degrees or radians, between two waves having the same frequency and referenced to the same point in time. Two oscillators that have the same frequency and no phase difference are said to be in phase. Two oscillators that have the same frequency and different phases have a phase difference, and the oscillators are said to be out of phase with each other.

The amount by which such oscillators are out of phase with each other can be expressed in degrees from 0° to 360°, or in radians from 0 to 2π. If the phase difference is 180 degrees (π radians), then the two oscillators are said to be in antiphase.

If two interacting waves meet at a point where they are in antiphase, then destructive interference will occur. It is common for waves of electromagnetic (light, RF), acoustic (sound) or other energy to become superposed in their transmission medium. When that happens, the phase difference determines whether they reinforce or weaken each other. Complete cancellation is possible for waves with equal amplitudes.

Time is sometimes used (instead of angle) to express position within the cycle of an oscillation. A phase difference is analogous to two athletes running around a race track at the same speed and direction but starting at different positions on the track. They pass a point at different instants in time. But the time difference (phase difference) between them is a constant - same for every pass since they are at the same speed and in the same direction. If they were at different speeds (different frequencies), the phase difference is undefined and would only reflect different starting positions. Technically, phase difference between two entities at various frequencies is undefined and does not exist.

• Time zones are also analogous to phase differences.

A real-world example of a sonic phase difference occurs in the warble of a Native American flute. The amplitude of different harmonic components of same long-held note on the flute come into dominance at different points in the phase cycle. The phase difference between the different harmonics can be observed on a spectrogram of the sound of a warbling flute.

Phase comparison

Phase comparison is a comparison of the phase of two waveforms, usually of the same nominal frequency. In time and frequency, the purpose of a phase comparison is generally to determine the frequency offset (difference between wave cycles) with respect to a reference.

A phase comparison can be made by connecting two signals to a two-channel oscilloscope. The oscilloscope will display two sine waves, as shown in the graphic to the right. In the adjacent image, the top sine wave is the test frequency, and the bottom sine wave represents a signal from the reference.

If the two frequencies were exactly the same, their phase relationship would not change and both would appear to be stationary on the oscilloscope display. Since the two frequencies are not exactly the same, the reference appears to be stationary and the test signal moves. By measuring the rate of motion of the test signal the offset between frequencies can be determined.

Vertical lines have been drawn through the points where each sine wave passes through zero. The bottom of the figure shows bars whose width represents the phase difference between the signals. In this case the phase difference is increasing, indicating that the test signal is lower in frequency than the reference.

Formula for phase of an oscillation or a wave

The phase of an oscillation or wave refers to a sinusoidal function such as the following:

${\displaystyle {\begin{aligned}x(t)&=A\cdot \cos(2\pi ft+\varphi )\\y(t)&=A\cdot \sin(2\pi ft+\varphi )=A\cdot \cos \left(2\pi ft+\varphi -{\tfrac {\pi }{2}}\right)\end{aligned}}}$

where ${\displaystyle \textstyle A}$, ${\displaystyle \textstyle f}$, and ${\displaystyle \textstyle \varphi }$ are constant parameters called the amplitude, frequency, and phase of the sinusoid. These functions are periodic with period ${\displaystyle \textstyle T={\frac {1}{f}}}$, and they are identical except for a displacement of ${\displaystyle \textstyle {\frac {T}{4}}}$ along the ${\displaystyle \textstyle t}$ axis. The term phase can refer to several different things:

• It can refer to a specified reference, such as ${\displaystyle \textstyle \cos(2\pi ft)}$, in which case we would say the phase of ${\displaystyle \textstyle x(t)}$ is ${\displaystyle \textstyle \varphi }$, and the phase of ${\displaystyle \textstyle y(t)}$ is ${\displaystyle \textstyle \varphi -{\frac {\pi }{2}}}$.
• It can refer to ${\displaystyle \textstyle \varphi }$, in which case we would say ${\displaystyle \textstyle x(t)}$ and ${\displaystyle \textstyle y(t)}$ have the same phase but are relative to their own specific references.
• In the context of communication waveforms, the time-variant angle ${\displaystyle \textstyle 2\pi ft+\varphi }$, or its principal value, is referred to as instantaneous phase, often just phase.

See also

• In-phase and quadrature components
• Instantaneous phase
• Lissajous curve
• Phase angle
• Phase cancellation
• Phase problem
• Phase velocity
• Phasor
• Polarization
• Coherence, the quality of a wave to display a well defined phase relationship in different regions of its domain of definition
• Absolute phase

References

1. ^ Cite error: The named reference phnist was invoked but never defined (see the help page).
2. ^ Ballou, Glen (2005). Handbook for sound engineers (3 ed.). Focal Press, Gulf Professional Publishing. p. 1499. ISBN 978-0-240-80758-4.
3. Clint Goss; Barry Higgins (2013). "The Warble". Flutopedia. Retrieved 2013-03-06.

External links

• "What is a phase?". Prof. Jeffrey Hass. "An Acoustics Primer", Section 8. Indiana University. © 2003. See also: (pages 1 thru 3. © 2013)
• Phase angle, phase difference, time delay, and frequency
• ECE 209: Sources of Phase Shift — Discusses the time-domain sources of phase shift in simple linear time-invariant circuits.
• Open Source Physics JavaScript HTML5
• Phase Difference Java Applet

• Wave mechanics
• Physical quantities