Sentences with phrase «as sqrt»

The point that systematic error propagates as sqrt -LSB-(sum - over-scatter) ^ 2 / (N - 1)-RSB--- where N is the number of measurements — follows from the fact that a degree of freedom is lost through the use of the mean measurement in calculating the systematic scatter.

Not exact matches

Gives examples of sqrt (2), pi and e as irrational numbers.

In the simplest case, if the mean increases as N then the standard deviation increases by N / sqrt (N) = sqrt (N).

The transfered power is the same at each layer so we can write T2 at some layer 2 at R2 in terms of T1 at layer 1 at R1 as T2 = T1sqrt (R1 / R2) so it is really a 1 / sqrt (R) dependence rather that sqrt (R) as I originally stated.

Note that despite the «wide» distribution of sqrt (Kv), the TCR and SLR distributions are not open - ended as shown in Figure 6 of Forest et al. (2008).

But the error in the distance grows with time, as [sqrt (t) * 1].

Aerosol cooling from volcanoes becomes irrelevant, etc. (ii) But even if I had based it on the point that averaging n times as many samples reduces the expected error by sqrt (n), what is «erroneous» about that?

When the inter-methodological (+ / --RRB- 2 C noted by Bemis, et al., is added as the rms to the average (+ / --RRB- 1.25 C measurement error from the work of McCrae 1950 and Bemis 1998, the combined 1 - sigma error in determined T = (+ / --RRB- sqrt (1.25 ^ 2 +2 ^ 2) = (+ / --RRB- 2.4 C.

That simplifies the discussion as then we can estimate \ (2 \ sigma \ approx 2 -LCB- \ sqrt -LCB- V / (N - 1)-RCB--RCB- \), where N is given by the number of uncorrelated Atlantic ocean areas between 20 ° N and 20 ° S. With a correlation length of ∼ 10 — 15 ° we obtain a rough estimate of N ≈ 12 for the tropical Atlantic sector.

If each point in the right slide is obtained as the average of 100 more or less normally distributed points in the left slide, the errors bars shrink by a factor of sqrt (100) = 10.

For very large s this simplifies to k = y» / (sqrt (s) * y» ³), which tends to zero as s tends to infinity, while for very small s it becomes k = sy», which again tends to zero but this time as s tends to zero instead of infinity.

As the internal measurement errors and the external inter-equational uncertainties stem from independent sets of systematic errors, they combine as the rms: (+ / --RRB- sqrt [measurement error) ^ 2 + (inter-equational spread) ^ 2] = sqrt -LSB-(1.25) ^ 2 + (1.75) ^ 2] = (+ / --RRB- 2.2 As the internal measurement errors and the external inter-equational uncertainties stem from independent sets of systematic errors, they combine as the rms: (+ / --RRB- sqrt [measurement error) ^ 2 + (inter-equational spread) ^ 2] = sqrt -LSB-(1.25) ^ 2 + (1.75) ^ 2] = (+ / --RRB- 2.2 as the rms: (+ / --RRB- sqrt [measurement error) ^ 2 + (inter-equational spread) ^ 2] = sqrt -LSB-(1.25) ^ 2 + (1.75) ^ 2] = (+ / --RRB- 2.2 C.

It decreases as 1 / sqrt (n), right?

But all that did not send Maxwell's equations to the dustbin of history; it is enshrined forever, in the velocity of light as c = 1 / sqrt (mu - naught x Epsilon - naught).

The number of free home - team skins awarded per match determined as follows: 2 * SQRT (N), where «N» equals the number of eligible participants (value $ 0).