Amplitude is the magnitude of change in the oscillating variable with each oscillation within an oscillating system. For example, sound waves in air are oscillations in atmospheric pressure and their amplitudes are proportional to the change in pressure during one oscillation. If a variable undergoes regular oscillations, and a graph of the system is drawn with the oscillating variable as the vertical axis and time as the horizontal axis, the amplitude is visually represented by the vertical distance between the extrema of the curve.
In older texts the phase is sometimes very confusingly called the amplitude.^{[1]}
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Peaktopeak amplitude is the change between peak (highest amplitude value) and trough (lowest amplitude value, which can be negative). With appropriate circuitry, peaktopeak amplitudes can be measured by meters or by viewing the waveform on an oscilloscope. Peaktopeak is a straightforward measurement on an oscilloscope, the peaks of the waveform being easily identified and measured against the graticule. This remains a common way of specifying amplitude, but sometimes other measures of amplitude are more appropriate.
In audio system measurements, telecommunications and other areas where the measurand is a signal that swings above and below a zero value but is not sinusoidal, peak amplitude is often used. This is the absolute value of the signal.
Semiamplitude means half the peaktopeak amplitude^{[2]}. It is the most widely used measure of orbital amplitude in astronomy and the measurement of small semiamplitudes of nearby stars is important in the search for exoplanets.^{[3]} For a sine wave, peak amplitude and semiamplitude are the same.
Some scientists^{[4]} use "amplitude" or "peak amplitude" to mean semiamplitude, that is, half the peaktopeak amplitude.^{[2]}
Root mean square (RMS) amplitude is used especially in electrical engineering: the RMS is defined as the square root of the mean over time of the square of the vertical distance of the graph from the rest state.^{[5]}
For complex waveforms, especially nonrepeating signals like noise, the RMS amplitude is usually used because it is both unambiguous and has physical significance. For example, the average power transmitted by an acoustic or electromagnetic wave or by an electrical signal is proportional to the square of the RMS amplitude (and not, in general, to the square of the peak amplitude).^{[6]}
For alternating current electrical power, the universal practice is to specify RMS values of a sinusoidal waveform. The peaktopeak voltage of a sine wave is nearly 3 times the RMS value, but is rarely used. Some common meter types used in electrical engineering are calibrated for RMS amplitude, but actually operate on a DC input. Both digital voltmeters and moving coil meters are in this category. Such meters require the AC input to be first rectified. They are not true RMS meters, but rather, are reading proportional to either rectified average or peak amplitude. The RMS calibration is only correct for a sine wave input since the ratio between peak, average and rms values is dependant on waveform. Until recently, true RMS meters were mostly used only in radio frequency measurements. These instruments based their measurement on detecting the heating effect in a load resistor with a thermistor. The advent of microprocessor controlled meters capable of calculating RMS by sampling the waveform has made true RMS measurement commonplace.
In general, the use of peak amplitude is simple and unambiguous only for symmetric periodic waves, like a sine wave, a square wave, or a triangular wave. For an asymmetric wave (periodic pulses in one direction, for example), the peak amplitude becomes ambiguous. This is because the value is different depending on whether the maximum positive signal is measured relative to the mean, the maximum negative signal is measured relative to the mean, or the maximum positive signal is measured relative to the maximum negative signal (the peaktopeak amplitude) and then divided by two. In electrical engineering, the usual solution to this ambiguity is to measure the amplitude from a defined reference potential (such as ground or 0V). Strictly speaking, this is no longer amplitude since there is the possibility that a constant (DC component) is included in the measurement.
In telecommunication, pulse amplitude is the magnitude of a pulse parameter, such as the voltage level, current level, field intensity, or power level.
Pulse amplitude is measured with respect to a specified reference and therefore should be modified by qualifiers, such as "average", "instantaneous", "peak", or "rootmeansquare".
Pulse amplitude also applies to the amplitude of frequency and phasemodulated waveform envelopes.^{[7]}
In this simple wave equation
x = A \sin(t  K) + b \ ,
A is the peak amplitude of the wave,
x is the oscillating variable,
t is time,
K and b are arbitrary constants representing time and displacement offsets respectively.
The units of the amplitude depend on the type of wave, but are always in the same units as the oscillating variable. A more general representation of the wave equation is more complex, but the role of amplitude remains analogous to this simple case.
For waves on a string, or in medium such as water, the amplitude is a displacement.
The amplitude of sound waves and audio signals (which relates to the volume) conventionally refers to the amplitude of the air pressure in the wave, but sometimes the amplitude of the displacement (movements of the air or the diaphragm of a speaker) is described. The logarithm of the amplitude squared is usually quoted in dB, so a null amplitude corresponds to −∞ dB. Loudness is related to amplitude and intensity and is one of most salient qualities of a sound, although in general sounds can be recognized independently of amplitude. The square of the amplitude is proportional to the intensity of the wave.
For electromagnetic radiation, the amplitude of a photon corresponds to the changes in the electric field of the wave. However radio signals may be carried by electromagnetic radiation; the intensity of the radiation (amplitude modulation) or the frequency of the radiation (frequency modulation) is oscillated and then the individual oscillations are varied (modulated) to produce the signal.
The amplitude may be constant (in which case the wave is a continuous wave) or may vary with time and/or position. The form of the variation of amplitude is called the envelope of the wave.
If the waveform is a pure sine wave, the relationships between peaktopeak, peak, mean, and RMS amplitudes are fixed and known, as they are for any continuous periodic wave. However, this is not true for an arbitrary waveform which may or may not be periodic or continuous.
For a sine wave the relationship between RMS and peaktopeak amplitude is:
\mbox{Peaktopeak} = 2 \sqrt{2} \times \mbox{RMS} \approx 2.8 \times \mbox{RMS} \, .
For other waveforms the relationships are not (necessarily) arithmetically the same as they are for sine waves.
Look up amplitude in Wiktionary, the free dictionary. 
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< Latin amplitudo < amplus (“‘large’”); see ample and tude.
Singular 
Plural 
amplitude (plural amplitudes)
Wikipedia ^{fr}
amplitude f. (plural amplitudes)
amplitude m. (definite singular amplituden; indefinite plural amplituder; definite plural amplitudene)
[[File:thumbthumb350pxIn this picture, y is the amplitude of the wave]]
The amplitude or peak amplitude of a wave is a measure of how big its oscillation is. Amplitudes are always positive numbers (for example: 3.5, 1, 120) and are never negative (for example: 3.5, 1, 120). Amplitudes are positive because distance can only be greater than zero or equal to zero; negative distance does not exist.
The distance from the top of one peak to the bottom of another is called peaktopeak amplitude. Another way to describe peaktopeak amplitude is to say that it is the distance between the maximum positive value and the maximum negative value of a wave.
