Frequency
Frequency  

Common symbols  f, ν 
SI unit  hertz (Hz) 
Other units 

In SI base units  s^{−1} 
Derivations from other quantities 

Dimension 
Frequency is the number of occurrences of a repeating event per unit of time.^{[1]} It is also occasionally referred to as temporal frequency for clarity, and is distinct from angular frequency. Frequency is measured in hertz (Hz) which is equal to one event per second. The period is the interval of time between events, so the period is the reciprocal of the frequency.^{[2]}
For example, if a heart beats at a frequency of 120 times a minute (2 hertz), the period, T—the interval at which the beats repeat—is half a second (60 seconds divided by 120 beats). Frequency is an important parameter used in science and engineering to specify the rate of oscillatory and vibratory phenomena, such as mechanical vibrations, audio signals (sound), radio waves, and light.
Definitions and units[edit]
For cyclical phenomena such as oscillations, waves, or for examples of simple harmonic motion, the term frequency is defined as the number of cycles or vibrations per unit of time. The conventional symbol for frequency is f; the Greek letter ν (nu) is also used.^{[3]} The period T is the time taken to complete one cycle of an oscillation or rotation. The relation between the frequency and the period is given by the equation^{[4]}
The term temporal frequency is used to emphasise that the frequency is characterised by the number of occurrences of a repeating event per unit time.
The SI unit of frequency is the hertz (Hz),^{[4]} named after the German physicist Heinrich Hertz by the International Electrotechnical Commission in 1930. It was adopted by the CGPM (Conférence générale des poids et mesures) in 1960, officially replacing the previous name, cycle per second (cps). The SI unit for the period, as for all measurements of time, is the second.^{[5]} A traditional unit of frequency used with rotating mechanical devices, where it is termed rotational frequency, is revolution per minute, abbreviated r/min or rpm.^{[6]} 60 rpm is equivalent to one hertz.^{[7]}
Period versus frequency[edit]
As a matter of convenience, longer and slower waves, such as ocean surface waves, are more typically described by wave period rather than frequency.^{[8]} Short and fast waves, like audio and radio, are usually described by their frequency. Some commonly used conversions are listed below:
Frequency  Period 

1 mHz (10^{−3} Hz)  1 ks (10^{3} s) 
1 Hz (10^{0} Hz)  1 s (10^{0} s) 
1 kHz (10^{3} Hz)  1 ms (10^{−3} s) 
1 MHz (10^{6} Hz)  1 μs (10^{−6} s) 
1 GHz (10^{9} Hz)  1 ns (10^{−9} s) 
1 THz (10^{12} Hz)  1 ps (10^{−12} s) 
Related quantities[edit]
 Angular frequency, usually denoted by the Greek letter ω (omega), is defined as the rate of change of angular displacement (during rotation), θ (theta), or the rate of change of the phase of a sinusoidal waveform (notably in oscillations and waves), or as the rate of change of the argument to the sine function: The unit of angular frequency is the radian per second (rad/s) but, for discretetime signals, can also be expressed as radians per sampling interval, which is a dimensionless quantity. Angular frequency is frequency multiplied by 2π.
 Spatial frequency, denoted here by ξ, is analogous to temporal frequency, but with a spatial measurement replacing time measurement,^{[note 1]} e.g.:
In wave propagation [edit]
For periodic waves in nondispersive media (that is, media in which the wave speed is independent of frequency), frequency has an inverse relationship to the wavelength, λ (lambda). Even in dispersive media, the frequency f of a sinusoidal wave is equal to the phase velocity v of the wave divided by the wavelength λ of the wave:
In the special case of electromagnetic waves in vacuum, then v = c, where c is the speed of light in vacuum, and this expression becomes
When monochromatic waves travel from one medium to another, their frequency remains the same—only their wavelength and speed change.
Measurement[edit]
Measurement of frequency can be done in the following ways:
Counting[edit]
Calculating the frequency of a repeating event is accomplished by counting the number of times that event occurs within a specific time period, then dividing the count by the period. For example, if 71 events occur within 15 seconds the frequency is:
Stroboscope[edit]
An old method of measuring the frequency of rotating or vibrating objects is to use a stroboscope. This is an intense repetitively flashing light (strobe light) whose frequency can be adjusted with a calibrated timing circuit. The strobe light is pointed at the rotating object and the frequency adjusted up and down. When the frequency of the strobe equals the frequency of the rotating or vibrating object, the object completes one cycle of oscillation and returns to its original position between the flashes of light, so when illuminated by the strobe the object appears stationary. Then the frequency can be read from the calibrated readout on the stroboscope. A downside of this method is that an object rotating at an integer multiple of the strobing frequency will also appear stationary.
Frequency counter[edit]
Higher frequencies are usually measured with a frequency counter. This is an electronic instrument which measures the frequency of an applied repetitive electronic signal and displays the result in hertz on a digital display. It uses digital logic to count the number of cycles during a time interval established by a precision quartz time base. Cyclic processes that are not electrical, such as the rotation rate of a shaft, mechanical vibrations, or sound waves, can be converted to a repetitive electronic signal by transducers and the signal applied to a frequency counter. As of 2018, frequency counters can cover the range up to about 100 GHz. This represents the limit of direct counting methods; frequencies above this must be measured by indirect methods.
Heterodyne methods[edit]
Above the range of frequency counters, frequencies of electromagnetic signals are often measured indirectly utilizing heterodyning (frequency conversion). A reference signal of a known frequency near the unknown frequency is mixed with the unknown frequency in a nonlinear mixing device such as a diode. This creates a heterodyne or "beat" signal at the difference between the two frequencies. If the two signals are close together in frequency the heterodyne is low enough to be measured by a frequency counter. This process only measures the difference between the unknown frequency and the reference frequency. To reach higher frequencies, several stages of heterodyning can be used. Current research is extending this method to infrared and light frequencies (optical heterodyne detection).
Examples[edit]
Light[edit]
Visible light is an electromagnetic wave, consisting of oscillating electric and magnetic fields traveling through space. The frequency of the wave determines its color: 400 THz (4×10^{14} Hz) is red light, 800 THz (8×10^{14} Hz) is violet light, and between these (in the range 400–800 THz) are all the other colors of the visible spectrum. An electromagnetic wave with a frequency less than 4×10^{14} Hz will be invisible to the human eye; such waves are called infrared (IR) radiation. At even lower frequency, the wave is called a microwave, and at still lower frequencies it is called a radio wave. Likewise, an electromagnetic wave with a frequency higher than 8×10^{14} Hz will also be invisible to the human eye; such waves are called ultraviolet (UV) radiation. Even higherfrequency waves are called Xrays, and higher still are gamma rays.
All of these waves, from the lowestfrequency radio waves to the highestfrequency gamma rays, are fundamentally the same, and they are all called electromagnetic radiation. They all travel through vacuum at the same speed (the speed of light), giving them wavelengths inversely proportional to their frequencies.
where c is the speed of light (c in vacuum or less in other media), f is the frequency and λ is the wavelength.In dispersive media, such as glass, the speed depends somewhat on frequency, so the wavelength is not quite inversely proportional to frequency.
Sound[edit]
Sound propagates as mechanical vibration waves of pressure and displacement, in air or other substances.^{[11]} In general, frequency components of a sound determine its "color", its timbre. When speaking about the frequency (in singular) of a sound, it means the property that most determines its pitch.^{[12]}
The frequencies an ear can hear are limited to a specific range of frequencies. The audible frequency range for humans is typically given as being between about 20 Hz and 20,000 Hz (20 kHz), though the high frequency limit usually reduces with age. Other species have different hearing ranges. For example, some dog breeds can perceive vibrations up to 60,000 Hz.^{[13]}
In many media, such as air, the speed of sound is approximately independent of frequency, so the wavelength of the sound waves (distance between repetitions) is approximately inversely proportional to frequency.
Line current[edit]
In Europe, Africa, Australia, southern South America, most of Asia, and Russia, the frequency of the alternating current in household electrical outlets is 50 Hz (close to the tone G), whereas in North America and northern South America, the frequency of the alternating current in household electrical outlets is 60 Hz (between the tones B♭ and B; that is, a minor third above the European frequency). The frequency of the 'hum' in an audio recording can show where the recording was made, in countries using a European, or an American, grid frequency.
Aperiodic frequency[edit]
Aperiodic frequency is the rate of incidence or occurrence of noncyclic phenomena, including random processes such as radioactive decay. It is expressed with the unit of reciprocal second (s^{−1})^{[14]} or, in the case of radioactivity, becquerels.^{[15]}
It is defined as a ratio, f = N/T, involving the number of times an event happened (N) during a given time duration (T); it is a physical quantity of type temporal rate.
See also[edit]
 Audio frequency
 Bandwidth (signal processing)
 Cutoff frequency
 Downsampling
 Electronic filter
 Fourier analysis
 Frequency band
 Frequency converter
 Frequency domain
 Frequency distribution
 Frequency extender
 Frequency grid
 Frequency modulation
 Frequency spectrum
 Interaction frequency
 Leastsquares spectral analysis
 Natural frequency
 Negative frequency
 Periodicity (disambiguation)
 Pink noise
 Preselector
 Radar signal characteristics
 Signaling (telecommunications)
 Spread spectrum
 Spectral component
 Transverter
 Upsampling
 Orders of magnitude (frequency)
Notes[edit]
 ^ The term spatial period, sometimes used in place of wavelength, analogously corresponds to the (temporal) period.^{[9]}
References[edit]
 ^ "Definition of FREQUENCY". Retrieved 3 October 2016.
 ^ "Definition of PERIOD". Retrieved 3 October 2016.
 ^ Serway & Faughn 1989, p. 346.
 ^ ^{a} ^{b} Serway & Faughn 1989, p. 354.
 ^ "Resolution 12 of the 11th CGPM (1960)". BIPM (International Bureau of Weights and Measures). Archived from the original on 8 April 2020. Retrieved 21 January 2021.
 ^ "Special Publication 811: NIST Guide to the SI, Chapter 8". Nist. 28 January 2016. Retrieved 20221108.
 ^ Davies 1997, p. 275.
 ^ Young 1999, p. 7.
 ^ Boreman, Glenn D. "Spatial Frequency". SPIE. Retrieved 22 January 2021.
 ^ Bakshi, K.A.; A.V. Bakshi; U.A. Bakshi (2008). Electronic Measurement Systems. US: Technical Publications. pp. 4–14. ISBN 9788184312065.^{[permanent dead link]}
 ^ "Definition of SOUND". Retrieved 3 October 2016.
 ^ Pilhofer, Michael (2007). Music Theory for Dummies. For Dummies. p. 97. ISBN 9780470167946.
 ^ Condon, Tim (2003). Elert, Glenn (ed.). "Frequency range of dog hearing". The Physics Factbook. Retrieved 20081022.
 ^ Lombardi, Michael A. (2007). "Fundamentals of Time and Frequency". In Bishop, Robert H. (ed.). Mechatronic Systems, Sensors, and Actuators: Fundamentals and Modeling. Austin: CRC Press. ISBN 9781420009002.
 ^ Newell, David B; Tiesinga, Eite (2019). The international system of units (SI): (PDF) (Report). Gaithersburg, MD: National Institute of Standards and Technology. doi:10.6028/nist.sp.3302019. sub§2.3.4, Table 4.
Sources[edit]
 Davies, A. (1997). Handbook of Condition Monitoring: Techniques and Methodology. New York: Springer. ISBN 9780412613203.
 Serway, Raymond A.; Faughn, Jerry S. (1989). College Physics. London: Thomson/BrooksCole. ISBN 9780534408145.
 Young, Ian R. (1999). Wind Generated Ocean Waves. Elsevere Ocean Engineering. Vol. 2. Oxford: Elsevier. ISBN 9780080433172.
Further reading[edit]
 Giancoli, D.C. (1988). Physics for Scientists and Engineers (2nd ed.). Prentice Hall. ISBN 9780136692010.