root mean square , RMS (skrót)

However, one can use the root mean square as a useful measure of that distance.

This process can be quite complex (see root mean square for a detailed mathematical explanation).

Even though it changes, the waveform has a root mean square (rms) value.

The root mean square is at least as high as the arithmetic mean, and usually higher.

Root mean square or better surface finish.

The quadratic mean (or root mean square) of these values is taken, similar to a standard deviation calculation.

Root mean square is important.

For the percentage format, root mean square (RMS) average is used.

Quantitative comparisons between different eyes and conditions are usually made using RMS (root mean square).

The effective sound pressure is the root mean square of the instantaneous sound pressure over a given interval of time.

The contraharmonic mean is higher in value than the average and also higher than the root mean square :

Statistical methods such as root mean square (RMS) duly address the "total" idea in this respect.

Voltages are expressed as root mean square (RMS) voltage.

The probability So that while the mean position after n steps is at the origin, the root mean square (r.m.s.) path length is.

There is also a harmonic average of functions and a quadratic average (or root mean square) of functions.

The second relationship is that the geometric mean of the arithmetic and contraharmonic means is the root mean square:

It should be borne in mind that this voltage is Root mean square, not peak, and also that it is only a nominal value.

Delay spread can be quantified through different metrics, although the most common one is the root mean square (rms) delay spread.

The root mean square is the square root of the arithmetic mean of the squares of the values.

Table 5.4 provides a summary of the overall fit in the form of the root mean squares (RMS) of the differences for each map.

Coefficient of variation and root mean square of successive differences were calculated for 100 R-R intervals free of artefacts.

The ex-post tracking error formula is the root mean square (RMS) of the active returns, given by:

These values typically include averages, maxima and minima, root mean square (RMS) and frequencies.

For example, the commonly used Root mean square (RMS) equation for gas reservoirs:

Correspondingly, one can define a granular temperature equal to the root mean square of grain velocity fluctuations that is analogous to thermodynamic temperature.