Root mean square

In mathematics, the root mean square (abbreviated RMS or rms), also known as the quadratic mean, is a statistical measure of the magnitude of a varying quantity. It is especially useful when variates are positive and negative, e.g., sinusoids.

It can be calculated for a series of discrete values or for a continuously varying function. The name comes from the fact that it is the square root of the mean of the squares of the values. It is a special case of the power mean with the exponent p = 2.


x_text{rms} = sqrt{ langle x_1^2 + x_2^2 + x_3^2 +...+ x_N^2 rangle/N} ,!

Ways of calculating the root mean square

The RMS of a collection of n values {x_1,x_2,dots,x_n} is

x_{mathrm{rms}} = sqrt {{1 over n} sum_{i=1}^{n} x_i^2} = sqrt {{x_1^2 + x_2^2 + cdots + x_n^2} over n}

The corresponding formula for a continuous function f(t) defined over the interval T_1 le t le T_2 is

f_{mathrm{rms}} = sqrt {int_{T_1}^{T_2} {[f(t)]}^2, dt}}

The RMS of a periodic function is equal to the RMS of one period of the function. The RMS value of a continuous function or signal can be approximated by taking the RMS of a series of equally spaced samples. Additionally, the RMS value of various waveforms can also be determined without calculus, as shown by Cartwright.


The RMS value of a function is often used in physics and electrical engineering.

Average electrical power

Engineers often need to know the power, P, dissipated by an electrical resistance, R. It is easy to do the calculation when there is a constant current, I, through the resistance. For a load of R ohms, power is defined simply as:

P = I^2 R.,!

However, if the current is a time-varying function, I(t), this formula must be extended to reflect the fact that the current (and thus the instantaneous power) is varying over time. If the function is periodic (such as household AC power), it is nonetheless still meaningful to talk about the average power dissipated over time, which we calculate by taking the simple average of the power at each instant in the waveform or, equivalently, the squared current. That is,

P_mathrm{avg},! = langle I(t)^2R rangle ,! (where langle ldots rangle denotes the mean of a function)
= Rlangle I(t)^2 rangle,! (as R does not vary over time it can be factored out)
= (I_mathrm{RMS})^2R,! (by definition of RMS)
So, the RMS value, I_mathrm{RMS}, of the function I(t) is the constant signal that yields the same average power dissipation.

We can also show by the same method that for a time-varying voltage, V(t), with RMS value V_mathrm{RMS},

P_mathrm{avg} = {(V_mathrm{RMS})^2over R}.,!

This equation can be used for any periodic waveform, such as a sinusoidal or sawtooth waveform, allowing us to calculate the mean power delivered into a specified load.

By taking the square root of both these equations and multiplying them together, we get the equation

P_mathrm{avg} = V_mathrm{RMS}I_mathrm{RMS}.,!

Both derivations depend on voltage and current being proportional (i.e., the load, R, is purely resistive). Reactive loads (i.e., loads capable of not just dissipating energy but also storing it) are discussed under the topic of AC power.

In the common case of alternating current when I(t) is a sinusoidal current, as is approximately true for mains power, the RMS value is easy to calculate from the continuous case equation above. If we define I_{mathrm{p}} to be the amplitude of the current, then:

I_{mathrm{RMS}} = sqrt {int_{T_1}^{T_2} {(I_mathrm{p}sin(omega t)}, })^2 dt}.,!

where t is time and ω is the angular frequency (ω = 2π/T, whereT is the period of the wave).

Since I_{mathrm{p}} is a positive constant:

I_{mathrm{RMS}} = I_mathrm{p}sqrt {int_{T_1}^{T_2} {sin^2(omega t)}, dt}}.

Using a trigonomentric identity to eliminate squaring of trig function:

I_{mathrm{RMS}} = I_mathrm{p}sqrt {int_{T_1}^{T_2} , dt}}

I_{mathrm{RMS}} = I_mathrm{p}sqrt left [{{t over 2} -{ sin(2omega t) over 4omega}} right ]_{T_1}^{T_2} }

but since the interval is a whole number of complete cycles (per definition of RMS), the sin terms will cancel, leaving:

I_{mathrm{RMS}} = I_mathrm{p}sqrt left [ right ]_{T_1}^{T_2} } = I_mathrm{p}sqrt {{{T_2-T_1} over 2}} } = {I_mathrm{p} over {sqrt 2}}.

A similar analysis leads to the analogous equation for voltage:

V_{mathrm{RMS}} = {V_mathrm{p} over {sqrt 2}}.

Because of their usefulness in carrying out power calculations, listed voltages for power outlets, e.g. 120 V (USA) or 230 V (Europe), are almost always quoted in RMS values, and not peak values. Peak values can be calculated from RMS values from the above formula, which implies Vp = VRMS × √2, assuming the source is a pure sine wave. Thus the peak value of the mains voltage in the USA is about 120 × √2, or about 170 volts. The peak-to-peak voltage, being twice this, is about 340 volts. A similar calculation indicates that the peak-to-peak mains voltage in Europe is about 650 volts.

It is also possible to calculate the RMS power of a signal. By analogy with RMS voltage and RMS current, RMS power is the square root of the mean of the square of the power over some specified time period. This quantity, which would be expressed in units of watts (RMS), has no physical significance. However, the term "RMS power" is sometimes used in the audio industry as a synonym for "mean power" or "average power". For a discussion of audio power measurements and their shortcomings, see Audio power.

Amplifier power efficiency

The electrical efficiency of an electronic amplifier is the ratio of mean output power to mean input power. As discussed, if the output is resistive, the mean output power can be found using the RMS values of output current and voltage signals. However, the mean value of the current should be used to calculate the input power. That is, the power delivered by the amplifier supplied by constant voltage V_{CC} is

P_mathrm{input}(t) = I_Q V_{CC} + I_mathrm{out}(t) V_{CC},
where I_Q is the amplifier's operating current. Clearly, because V_{CC} is constant, the time average of P_mathrm{input} depends on the time average value of I_mathrm{out} and not its RMS value. That is,
langle P_mathrm{input}(t) rangle = I_Q V_{CC} + langle I_mathrm{out}(t) rangle V_{CC},

Root mean square velocity

In physics, the root mean square velocity is defined as the square root of the average velocity-squared of the molecules in a gas. The RMS velocity of an ideal gas is calculated using the following equation:

{v_mathrm{RMS}} = {sqrt{3RT over {M}}}

where R represents the ideal gas constant (in this case, 8.314 J/(mol⋅K)), T is the temperature of the gas in kelvins, and M is the molar mass of the compound in kilograms per mole. Note that the unit of mass is in kilograms per mole because the joule is given in kilogram meters squared per second squared.

Relationship to the arithmetic mean and the standard deviation

If bar{x} is the arithmetic mean and sigma_{x} is the standard deviation of a population (the equation is different when sigma_{x} is for a sample) then:
x_{mathrm{rms}}^2 = bar{x}^2 + sigma_{x}^2.

From this it is clear that the RMS value is always greater than or equal to the average, in that the RMS includes the "error" / square deviation as well.

Physical scientists often use the term "root mean square" as a synonym for standard deviation when referring to the square root of the mean squared deviation of a signal from a given baseline or fit. This is useful for electrical engineers in calculating the "AC only" RMS of a signal. Standard deviation being the root mean square of a signal's variation about the mean, rather than about 0, the DC component is removed (i.e. RMS(signal) = Stdev(signal) if the mean signal is 0).

See also


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