Chapter 19: Measures of Dispersion
Two districts may record the same average annual rainfall, and yet cultivation in one of them is far more secure than in the other. In the first, the rain arrives in a steady spread across the monsoon months. In the second, the same total falls in a few violent spells, with long dry stretches in between. The average conceals the difference completely. The measures of central value studied earlier showed how a single figure — the mean, the median or the mode — can be made to stand for a whole set of observations. That figure tells us where the data centre, but nothing at all about how closely the observations gather around that centre. Two series with the same average may be almost alike, or quite unlike each other. To describe a set of data honestly, and to know how far the average may be trusted as a representative of it, we need a second measure alongside the average: a measure of the spread, or dispersion, of the observations. This chapter explains what dispersion is, how it is measured by range, quartile deviation, mean deviation and standard deviation, and how two series are compared by the coefficient of variation.
Fig. 19.0 – Two series with the same average but different spread.
19.1 The Need to Measure Dispersion
19.1.1 Why an Average Is Not Enough
A measure of central value condenses a large body of data into a single figure. That figure is representative in the sense that the observations cluster about it, and it allows two series to be compared at a glance. Statistics would be unmanageable without such condensation.
But condensation always costs information. The average records where the observations centre; it records nothing about how tightly or loosely they are gathered around that centre. Two series may share an average and yet describe quite different situations.
Suppose the number of children in four families is recorded in each of three colonies, as set out in Table 19.1. Every colony has twelve children in all, and so an average of three children per family.
The three averages are identical, but the three colonies are not. In Colony X every family has exactly three children, so the average describes each family perfectly. In Colony Y the families differ, though not greatly. In Colony Z one family has eight children while two have only one, and the average of three describes no family in the colony at all.
The average is therefore a reliable representative in Colony X and a poor one in Colony Z. Whether an average can be trusted depends on how far the individual observations lie from it — and that is a second and independent property of the data, which must be measured separately.
19.1.2 Meaning of Dispersion
The scatter of the observations about the average is called dispersion, or variation. Where the observations lie close to the average, dispersion is low and the series is said to be uniform or homogeneous. Where they lie far from it, dispersion is high and the series is heterogeneous.
Dispersion is thus a property of the whole set of observations, not of any one of them. It is always measured with reference to some average, and the measures studied in this chapter differ chiefly in which average they are measured from and how the distances from it are treated.
19.1.3 Objectives of Measuring Dispersion
Dispersion is measured for four main reasons.
- To judge the reliability of the average — a low dispersion means the average is close to most of the observations and can be trusted to represent them, while a high dispersion warns that the average stands for very few of the items actually observed.
- To describe the composition of a series — the average and the dispersion taken together tell us both where the data centre and how they are distributed about that centre, which neither figure conveys on its own.
- To compare two or more series — two series with the same average may still differ in uniformity, and a comparison of averages alone would miss that difference entirely.
- To control variation — once the extent of variation is measured, its causes can be investigated, and where variation is undesirable it can be reduced.
19.1.4 Usefulness of Dispersion
The study of dispersion has wide application in economics and in business.
- Income and wealth — the extent of inequality in an economy is a question about the dispersion of incomes, since average income alone cannot show how unequally that income is shared.
- Quality control — parts manufactured separately must be assembled later, so a producer needs the variation in their sizes to stay within narrow limits, whatever the average size may be.
- Productivity — variation in output per worker across a workshop directs the manager’s attention to the causes of that variation rather than to the average alone.
- Financial markets — the variability of the price of a share or a bond is taken as a measure of the risk carried by the person who holds it.
- Further statistical work — correlation, regression and the theory of sampling all rest on measures of dispersion, so the study of dispersion is a step towards the techniques that follow it.
19.1.5 Properties of a Good Measure of Dispersion
Several measures of dispersion are in use, and they do not all serve equally well. A good measure should satisfy the following conditions.
- Rigidly defined — the measure should be defined precisely, so that every person computing it from the same data arrives at the same value.
- Easy to understand and simple to calculate — a measure that is laborious or obscure will not be used, however sound it may be in principle.
- Based on all the observations — a measure that ignores most of the data cannot reflect the variation present in them.
- Not unduly affected by extreme values — one unusually large or small observation should not be allowed to dominate the result.
- Stable across samples — the measure should not vary widely between different samples drawn from the same population.
- Capable of algebraic treatment — where the measure is known for two parts of a set of data, it should be possible to obtain the measure for the whole.
No single measure satisfies every one of these conditions. The merits and demerits of each measure, examined in the sections that follow, are best read as a record of which conditions it meets and which it fails.
19.2 Types of Measures of Dispersion
Dispersion can be measured in more than one way, and the measures fall into two families. The first states the scatter in the units in which the data themselves are recorded. The second states it as a ratio, free of any unit. The whole classification is set out in Fig. 19.1.
Fig. 19.1 – Classification of the measures of dispersion.
19.2.1 Absolute Measures of Dispersion
An absolute measure states the scatter in the same unit as the original data. If the data are daily wages in rupees, the measure is a number of rupees; if they are heights in centimetres, it is a number of centimetres.
Because the unit survives the calculation, an absolute measure can be read directly and reported as it stands. It is the natural choice whenever a single distribution is under study and no comparison with another distribution is intended.
19.2.2 Relative Measures of Dispersion
The unit that makes an absolute measure easy to read also makes it useless for comparison. A scatter of ₹40 in the wages of one factory cannot be set against a scatter of 6 centimetres in the heights of its workers, because rupees and centimetres cannot be compared at all. Even two series in the same unit are not safely compared by an absolute measure if their averages are far apart: a variation of ₹5 means one thing in the price of a kilogram of onions and quite another in the price of a gram of gold.
The remedy is to divide the absolute measure by an average of the same series. The unit then cancels, and what remains is a pure number that can be set beside the corresponding figure for any other series.
\[\text{Relative measure of dispersion} = \dfrac{\text{Absolute measure of dispersion}}{\text{Average of the series}}\]
Here the absolute measure and the average are both in the units of the original data, so the ratio has no unit at all. A larger value means greater variation relative to the size of the observations themselves.
A relative measure of dispersion is also called a coefficient of dispersion. Each of the four absolute measures has its own coefficient, and the coefficient of variation, taken up in §19.7, is a fifth relative measure obtained from the standard deviation.
The main points of difference are set out below.
19.2.3 Distance Measures and Average Deviation Measures
The four absolute measures divide again, this time by the method they use to arrive at a figure for the scatter.
- Distance measures — these take the distance between two values in the series and treat that distance as the measure of the scatter. The larger the distance, the greater the variation. Range and quartile deviation are distance measures.
- Average deviation measures — these find how far each observation lies from an average of the series, and then average those distances. Every observation contributes to the result. Mean deviation and standard deviation are average deviation measures.
The distinction matters because it explains the merits and demerits met later in the chapter. A distance measure is quick to compute but rests on two values only, so it ignores everything that lies between them. An average deviation measure uses the whole series and is correspondingly more representative, but it takes longer to compute and is more sensitive to observations lying far from the centre.
19.2.4 The Four Measures Studied in This Chapter
The syllabus requires four absolute measures, their coefficients, and the coefficient of variation. They are taken up in turn.
- Range — the difference between the largest and the smallest observation in the series.
- Quartile deviation — half the distance between the third quartile and the first quartile, so that it measures the spread of the middle half of the data.
- Mean deviation — the average of the distances of the observations from the mean or from the median, the signs of those distances being ignored.
- Standard deviation — the square root of the average of the squared distances of the observations from the arithmetic mean.
Each section defines the measure, works it out for individual, discrete and continuous series, gives its coefficient, and closes with its merits and demerits.
19.3 Range
19.3.1 Meaning of Range
The simplest question that can be asked about the scatter of a series is how far apart its two extreme observations lie. The answer is the range.
Range measures the total spread of the data from one end to the other. It states the width of the interval within which every observation of the series must fall, and says nothing about how the observations are distributed inside that interval.
\[R = H - L\]
Here \(R\) is the range, \(H\) the highest value observed in the series and \(L\) the lowest value observed. The result carries the unit of the original data, so the range of a wage series is in rupees and the range of a height series in centimetres. A larger value of \(R\) means a wider spread.
Fig. 19.2 shows what the measure captures and what it leaves out.
Fig. 19.2 – Range as the distance between the two extreme values.
19.3.2 Range in an Individual Series
In an individual series the observations are listed one by one. The largest and the smallest are read off directly and subtracted. Arranging the data in ascending order first is not strictly necessary, but it makes the two extreme values easy to identify and guards against error.
19.3.3 Range in a Discrete Series
A discrete series records each value of the variable along with the number of times it occurs. The range is found exactly as in an individual series: the smallest value of the variable is subtracted from the largest. The frequencies are not used at all, because the range is a statement about which values occur, not about how often they occur. The data of the following example are set out in Table 19.2.
19.3.4 Range in a Continuous Series
In a continuous series the individual observations are lost inside class intervals, so the highest and lowest values are not directly available. Two methods are in use, and they do not give the same answer.
- Method 1 — take the difference between the mid-value of the highest class and the mid-value of the lowest class.
- Method 2 — take the difference between the upper class boundary of the highest class and the lower class boundary of the lowest class.
Method 1 treats the mid-value as representative of its class, which is the convention followed everywhere else in the treatment of grouped data. Method 2 takes the outer limits of the distribution and therefore always gives the larger figure, exceeding Method 1 by exactly one class width.
Where the classes are inclusive — that is, where one class ends at 249 and the next begins at 250 — the class boundaries must be found before Method 2 can be applied. The gap between the two classes is divided equally, half a unit being subtracted from the lower limit and added to the upper limit of each class. Method 1 needs no such conversion, since the mid-value of a class is unchanged by it. The distribution used below is set out in Table 19.3.
19.3.5 Coefficient of Range
Range carries the unit of the data, so the ranges of two series cannot be compared unless the series are measured in the same unit and have averages of much the same size. The relative measure that removes this difficulty is the coefficient of range.
There is no average of the range itself to divide by, so the sum of the two extreme values is used in its place.
\[\text{Coefficient of range} = \dfrac{H - L}{H + L}\]
Here \(H\) and \(L\) are again the highest and lowest values of the series. Both numerator and denominator carry the same unit, so the coefficient is a pure number. It lies between 0 and 1, and the closer it is to 1, the greater the variation relative to the size of the observations themselves. The two series compared below are given in Table 19.4.
19.3.6 Merits of Range
- Easy to understand — the meaning of the largest value less the smallest is plain to anyone, which is why the range is the measure most often quoted outside statistics.
- Simple to calculate — it needs only two observations and a single subtraction, and no average has to be found first.
- Useful where the limits matter — in quality control, in the reporting of price and temperature movements, and in setting tolerance limits, it is precisely the outer bounds of the variation that are wanted.
19.3.7 Demerits of Range
- Not rigidly defined — for a continuous series two accepted methods exist and give different answers, so the same data can yield more than one range.
- Not based on all the observations — only the two extreme values enter the calculation, and the distribution of everything between them is ignored entirely.
- Unduly affected by extreme values — a single unusually high or low observation raises the range sharply, though the rest of the series may be closely packed.
- Unstable across samples — because it rests on two observations, the range differs widely between samples drawn from the same population.
- Not applicable to open-ended distributions — where the first or last class has no stated limit, neither method can be applied.
These demerits are serious enough that the range is rarely used as the only measure of dispersion. It is best treated as a first, rough indication of spread, to be followed by a measure that takes the whole series into account.
19.4 Quartile Deviation
19.4.1 Quartiles and the Interquartile Range
The weakness of the range is that its two extreme values are exactly the observations least likely to be typical. A measure that ignores the outer portions of the data and reports the spread of the central portion instead escapes that weakness. The quartiles provide the dividing points.
The three quartiles are written \(Q_1\), \(Q_2\) and \(Q_3\). The first quartile \(Q_1\), called the lower quartile, is the value below which one-fourth of the observations lie. The second quartile \(Q_2\) is the value below which one-half of them lie, and is therefore the median. The third quartile \(Q_3\), called the upper quartile, is the value below which three-fourths of the observations lie. Their position in the series is shown in Fig. 19.3.
Fig. 19.3 – Quartiles dividing a series into four equal parts.
The distance between the upper and the lower quartile is the interquartile range.
\[\text{Interquartile range} = Q_3 - Q_1\]
Since one-fourth of the observations lie below \(Q_1\) and one-fourth above \(Q_3\), this distance spans the middle half of the series. It carries the unit of the original data, and a larger value means the central half of the observations is more widely spread.
19.4.2 Meaning of Quartile Deviation
The interquartile range measures the spread of half the observations, so halving it gives a figure comparable to a deviation on either side of the centre. That figure is the quartile deviation.
\[QD = \dfrac{Q_3 - Q_1}{2}\]
Here \(QD\) is the quartile deviation and \(Q_3\) and \(Q_1\) are the upper and lower quartiles. The result is in the units of the data. It is read as the average distance of the two quartiles from the median, so a quartile deviation of ₹40 says that the middle half of the series lies roughly within ₹40 on either side of the median.
Quartile deviation is a distance measure, like the range. It differs from the range in the two values whose distance it takes: not the extreme observations, but the two points that cut off the outer quarters of the data.
19.4.3 Quartile Deviation in an Individual Series
The observations are first arranged in ascending order. The positions of the two quartiles are then located by the following rules.
\[Q_1 = \text{size of } \left(\dfrac{N+1}{4}\right)\text{th item} \qquad Q_3 = \text{size of } \dfrac{3(N+1)}{4}\text{th item}\]
Here \(N\) is the number of observations. The two expressions give positions in the ordered array, not values: the value standing at that position is the quartile. Where the position works out to a whole number the value is read off directly, and where it is fractional the quartile lies between two adjacent observations and is estimated approximately.
19.4.4 Quartile Deviation in a Discrete Series
In a discrete series the same positional formulas are used, with \(N\) taken as the total frequency \(\Sigma f\). The positions are located against a column of cumulative frequencies: the quartile is the value of the variable against the first cumulative frequency that equals or exceeds the required position. The cumulative frequencies for the following example are worked out in Table 19.5.
19.4.5 Quartile Deviation in a Continuous Series
In a continuous series the observations are grouped, so a quartile cannot be read off as the value of a particular item. The class in which the quartile falls is located first, and its value inside that class is then estimated by interpolation. Because the variable is treated as continuous, the positions are taken as the \(\dfrac{N}{4}\)th and \(\dfrac{3N}{4}\)th items rather than the \(\dfrac{N+1}{4}\)th and \(\dfrac{3(N+1)}{4}\)th.
\[Q_1 = l_1 + \dfrac{\dfrac{N}{4} - c.f.}{f} \times C \qquad Q_3 = l_1 + \dfrac{\dfrac{3N}{4} - c.f.}{f} \times C\]
Here \(l_1\) is the lower limit of the class in which the quartile lies, \(c.f.\) the cumulative frequency of the class preceding it, \(f\) the frequency of the quartile class itself, \(C\) the size of that class, and \(N\) the total frequency. The result carries the unit of the variable. The distribution and its cumulative frequencies are set out in Table 19.6.
19.4.6 Coefficient of Quartile Deviation
Quartile deviation carries the unit of the data and cannot be compared across series measured differently. Dividing the interquartile range by the sum of the two quartiles removes the unit and gives the coefficient of quartile deviation.
\[\text{Coefficient of } QD = \dfrac{Q_3 - Q_1}{Q_3 + Q_1}\]
Here \(Q_3\) and \(Q_1\) are the two quartiles. Numerator and denominator carry the same unit, so the coefficient is a pure number lying between 0 and 1. The larger it is, the greater the variation in the central half of the data relative to the level of the observations.
19.4.7 Merits of Quartile Deviation
- Simple to understand and calculate — it requires only the two quartiles, and no deviation has to be taken from an average.
- Not affected by extreme values — the highest and lowest quarters of the data are set aside altogether, so an unusually large or small observation cannot influence the result.
- Usable with open-ended distributions — the quartiles lie inside the closed classes, so the measure can be computed where range and standard deviation cannot.
- Suited to the central portion of the data — where interest lies in how the typical half of a series is spread, it answers exactly that question.
19.4.8 Demerits of Quartile Deviation
- Not rigidly defined — where the quartile position works out to a fraction, the quartile itself is only approximated, and different conventions yield slightly different values.
- Not based on all the observations — it uses two values only and ignores the outer half of the data entirely, so it is less representative than a measure built from the whole series.
- Unstable across samples — resting on two values, it differs from one sample to another drawn from the same population.
- Not capable of algebraic treatment — quartile deviations of two parts of a set of data cannot be combined to give the quartile deviation of the whole.
Quartile deviation is therefore an improvement on the range, since it discards the extreme observations rather than depending on them, but it shares the range’s basic limitation of resting on two values only. A measure that uses every observation is taken up next.
19.5 Mean Deviation
19.5.1 Meaning of Mean Deviation
Range and quartile deviation each rest on two values. A measure that reflects the whole series must begin from every observation, and the natural way to do that is to ask how far each observation lies from the average and then to average those distances.
One difficulty appears at once. The deviations from the arithmetic mean are positive for observations above the mean and negative for those below it, and the two sets exactly cancel: the sum of the deviations from the arithmetic mean is always zero. Averaging them would give zero for every series, however scattered. Fig. 19.4 shows why.
Fig. 19.4 – Deviations from the mean must be taken without signs.
The signs are accordingly dropped, and the absolute values of the deviations are averaged instead. The result is the mean deviation.
Because the sign is discarded, mean deviation states how far a typical observation lies from the average, in either direction. It may be computed from the arithmetic mean or from the median, and the two give different answers, so the average used must always be stated. Of the two, the mean deviation taken from the median is the smaller.
19.5.2 Mean Deviation in an Individual Series
Each observation’s distance from the chosen average is found, the signs are dropped, and the arithmetic mean of those distances is taken.
\[MD_{\bar{x}} = \dfrac{\Sigma |X - \bar{x}|}{N} \qquad MD_{m} = \dfrac{\Sigma |X - M|}{N}\]
Here \(X\) is an observation, \(\bar{x}\) the arithmetic mean, \(M\) the median, and \(N\) the number of observations. The vertical bars mean that the deviation is taken as a positive quantity whatever its sign. The result carries the unit of the original data. The deviations from both averages are worked out in Table 19.7.
19.5.3 Mean Deviation in a Discrete Series
Where each value occurs more than once, its deviation must count once for every occurrence. Each absolute deviation is therefore multiplied by the frequency of its value, and the total is divided by the total frequency.
\[MD_{\bar{x}} = \dfrac{\Sigma f|X - \bar{x}|}{\Sigma f} \qquad MD_{m} = \dfrac{\Sigma f|X - M|}{\Sigma f}\]
Here \(f\) is the frequency of the value \(X\), and the other symbols carry the meanings already given. The working for the following distribution is set out in Table 19.8.
19.5.4 Mean Deviation in a Continuous Series
In a continuous series the individual observations are not available, so the mid-value of each class is taken to represent every observation in it. Beyond that substitution the procedure is exactly that of a discrete series.
\[MD_{\bar{x}} = \dfrac{\Sigma f|m - \bar{x}|}{\Sigma f}\]
Here \(m\) is the mid-value of a class and \(f\) its frequency. The arithmetic mean is itself computed from the mid-values as \(\bar{x} = \dfrac{\Sigma fm}{\Sigma f}\). The working is set out in Table 19.9.
19.5.5 Coefficient of Mean Deviation
Mean deviation carries the unit of the data, so the relative measure is obtained by dividing it by the same average the deviations were taken from. This is the coefficient of mean deviation.
\[\text{Coefficient of } MD_{\bar{x}} = \dfrac{MD_{\bar{x}}}{\bar{x}} \qquad \text{Coefficient of } MD_{m} = \dfrac{MD_{m}}{M}\]
Here \(MD_{\bar{x}}\) and \(MD_{m}\) are the mean deviations from the mean and the median, and \(\bar{x}\) and \(M\) are those two averages. The unit cancels, leaving a pure number. The divisor must match the average used in computing the mean deviation: a mean deviation taken from the median is divided by the median, never by the mean.
19.5.6 Merits of Mean Deviation
- Based on all the observations — every item enters the calculation, so the measure reflects the whole series and not merely its extremes or its central half.
- Simple to understand — it is the average distance from an average, which is exactly what the ordinary idea of scatter means.
- Less affected by extreme values than standard deviation — the deviations are taken as they stand rather than squared, so an unusually distant observation does not dominate the result.
- Flexible in the average used — it can be computed about the mean or about the median, whichever suits the data.
19.5.7 Demerits of Mean Deviation
- Not well defined — since it may be taken from the mean or from the median, the same data yield more than one mean deviation, and the figure is meaningless unless the average used is stated.
- Non-algebraic in nature — ignoring the signs of the deviations is a mathematical device rather than a sound operation, and it makes the measure unsuitable for further algebraic work.
- Not capable of algebraic treatment — the mean deviations of two parts of a set of data cannot be combined to give the mean deviation of the whole.
- Little used in advanced work — techniques such as correlation and regression are built on squared deviations, so mean deviation has no place in them.
Mean deviation therefore corrects the chief weakness of the two distance measures by using every observation, but it removes the signs of the deviations by discarding them. The measure taken up next removes them by squaring instead, and that single change makes it the most widely used measure of dispersion.
19.6 Standard Deviation
19.6.1 Meaning of Standard Deviation
Mean deviation disposed of the signs of the deviations by ignoring them. That works arithmetically but not algebraically, and it is the reason the measure leads nowhere beyond itself. There is a second way of removing a sign: squaring. The square of a negative number is positive, and squaring, unlike the dropping of a sign, is an operation that can be carried through the rest of a calculation.
Squaring the deviations, averaging the squares, and then taking the square root to return to the original unit gives the standard deviation.
Standard deviation is always computed from the arithmetic mean, never from the median or the mode, so the ambiguity that troubles mean deviation does not arise. It is denoted by the Greek letter \(\sigma\), read sigma, and because it is the root of a mean of squares it is also called the root mean square deviation. The result carries the unit of the original data, and a larger \(\sigma\) means the observations lie further from their mean.
19.6.2 Standard Deviation in an Individual Series
Two methods are in use. Both give the same answer; they differ only in the value the deviations are taken from.
19.6.2.1 Direct Method
The deviations are taken from the actual arithmetic mean.
\[\sigma = \sqrt{\dfrac{\Sigma x^2}{N}}\]
Here \(x = X - \bar{x}\) is the deviation of an observation from the arithmetic mean, \(\Sigma x^2\) the total of the squared deviations, and \(N\) the number of observations. The square root returns the answer to the unit of the original data. The working is set out in Table 19.10.
19.6.2.2 Short-Cut Method
Where the arithmetic mean is not a whole number, deviations taken from it are awkward and every square becomes laborious. The short-cut method takes deviations from a convenient assumed mean instead, and corrects for the difference at the end.
\[\sigma = \sqrt{\dfrac{\Sigma d^2}{N} - \left(\dfrac{\Sigma d}{N}\right)^2}\]
Here \(d = X - A\) is the deviation of an observation from the assumed mean \(A\), which may be any value in or near the series. The term subtracted is the correction for the gap between the assumed mean and the true mean, and it is what makes the two methods agree. The working is set out in Table 19.11.
19.6.3 Standard Deviation in a Discrete Series
Each squared deviation is weighted by the frequency of its value, and the total is divided by the total frequency.
\[\sigma = \sqrt{\dfrac{\Sigma fx^2}{\Sigma f}}\]
Here \(f\) is the frequency of the value \(X\), \(x = X - \bar{x}\) the deviation of that value from the arithmetic mean, and \(\Sigma f = N\) the total frequency. The short-cut form for a discrete series replaces \(x\) by \(d = X - A\) and adds the same correction as before. The working is set out in Table 19.12.
19.6.4 Standard Deviation in a Continuous Series
19.6.4.1 Direct and Short-Cut Methods
In a continuous series the mid-value of each class stands for every observation in it, and the two methods already given are applied to those mid-values.
\[\sigma = \sqrt{\dfrac{\Sigma fx^2}{N}} \qquad \sigma = \sqrt{\dfrac{\Sigma fd^2}{N} - \left(\dfrac{\Sigma fd}{N}\right)^2}\]
Here \(x = m - \bar{x}\) and \(d = m - A\), where \(m\) is the mid-value of a class, and \(N = \Sigma f\). Nothing else changes.
19.6.4.2 Step Deviation Method
Where the classes are of equal size, the deviations from the assumed mean are all multiples of the class size, and dividing them by it reduces every figure to a small whole number. This is the step deviation method, and it is the one ordinarily used for grouped data.
\[\sigma = \sqrt{\dfrac{\Sigma fd'^2}{N} - \left(\dfrac{\Sigma fd'}{N}\right)^2} \times C\]
Here \(d' = \dfrac{m - A}{C}\) is the step deviation, \(C\) the common class size, \(A\) the assumed mean and \(N = \Sigma f\). Dividing by \(C\) shrinks every deviation, so the final multiplication by \(C\) restores the answer to the unit of the original data. The arithmetic mean itself is obtained from the same columns as \(\bar{x} = A + \dfrac{\Sigma fd'}{N} \times C\). The working is set out in Table 19.13.
19.6.5 Coefficient of Standard Deviation
Standard deviation carries the unit of the data. Dividing it by the arithmetic mean of the same series removes the unit and gives the coefficient of standard deviation.
\[\text{Coefficient of } SD = \dfrac{\sigma}{\bar{x}}\]
Here \(\sigma\) is the standard deviation and \(\bar{x}\) the arithmetic mean. Both carry the same unit, so the coefficient is a pure number, and the larger it is, the greater the variation relative to the size of the observations. Expressed as a percentage, this same ratio becomes the coefficient of variation, taken up in §19.7.
19.6.6 Merits of Standard Deviation
- Rigidly defined — it is computed from the arithmetic mean by one method only, so the same data always yield the same value.
- Based on all the observations — every item contributes a squared deviation, and the measure therefore reflects the whole series.
- Capable of algebraic treatment — standard deviations of two parts of a set of data can be combined to give the standard deviation of the whole, which no other measure in this chapter permits.
- Stable across samples — it is affected less by sampling fluctuations than the range or the quartile deviation.
- Basis of further statistical work — correlation, regression and the theory of sampling all rest on it, so it is the measure that leads somewhere beyond itself.
19.6.7 Demerits of Standard Deviation
- Difficult to compute — squaring every deviation and extracting a root make it the most laborious of the four measures, and the least easily explained to a reader without training.
- Gives more weight to extreme values — squaring magnifies the large deviations more than the small ones, so an observation far from the mean influences the result out of proportion to its number.
These two demerits are real but slight beside the merits. Standard deviation is accordingly the measure of dispersion in ordinary use wherever the data allow it to be computed.
19.7 Coefficient of Variation
19.7.1 Meaning of the Coefficient of Variation
Standard deviation is the most satisfactory of the absolute measures, but it carries the unit of the data and so cannot be set against the standard deviation of a series measured differently. Even two series in the same unit are not safely compared by it if their averages are far apart, since a scatter of ₹50 means one thing about a wage of ₹200 and quite another about a wage of ₹2,000.
The coefficient of standard deviation, met in §19.6.5, removes the unit by dividing \(\sigma\) by the mean. Multiplying that ratio by 100 expresses it as a percentage, and the result is the coefficient of variation.
\[CV = \dfrac{\sigma}{\bar{x}} \times 100\]
Here \(\sigma\) is the standard deviation of the series and \(\bar{x}\) its arithmetic mean. The two carry the same unit, which cancels, so the coefficient of variation is a pure number stated in per cent. It says how large the scatter is as a proportion of the average about which that scatter occurs.
A high coefficient of variation means the observations are widely spread relative to their own average: the series is variable, unstable, and its average is a weak representative of it. A low coefficient means the observations cluster closely about their average: the series is consistent, stable and uniform, and its average can be trusted.
19.7.2 Comparing the Variability of Two Series
The coefficient of variation earns its place when two series must be compared. Because it is a pure number, the comparison holds whether the two series are measured in the same unit or in different ones, and whatever the gap between their averages.
The conclusion drawn from it can differ from the conclusion the standard deviations alone would suggest. A series with the larger standard deviation may still be the more consistent of the two, if its average is larger in proportion. The working for the following comparison is set out in Table 19.14.
Where the two series are measured in different units, the standard deviations cannot be compared at all and the coefficient of variation is the only measure available.
19.8 Choosing a Measure of Dispersion
Four measures of dispersion have been worked out on the same kinds of data, and they do not agree with one another. That is not a defect. Each answers a slightly different question about the scatter, and the properties set out in §19.1.5 are met by each of them only in part. Choosing between them means knowing which properties matter for the work in hand.
19.8.1 Range and Quartile Deviation Compared
Both are distance measures: each takes two values from the series and reports the gap between them. They differ in which two values they take, and everything else follows from that. The main points of difference are set out below.
Quartile deviation is thus the better measure of the two wherever the extreme observations are unreliable, unrepresentative or simply missing. Range remains useful where the extremes are precisely what is wanted, as in quality control or in reporting the day’s highest and lowest price.
19.8.2 Mean Deviation and Standard Deviation Compared
Both are average deviation measures: each finds how far the observations lie from an average and then averages those distances. They differ in how the signs of the deviations are disposed of, and that single difference accounts for the standing of the two measures.
Standard deviation is accordingly the measure used wherever the data permit. Mean deviation survives as the simpler and more directly intelligible of the two, and as the measure less distorted by an observation lying far from the centre.
19.8.3 Which Measure to Use
No measure is best in the abstract. The choice turns on three questions: what the data allow, what degree of accuracy the purpose demands, and whether one series or two are being examined.
- What the data allow — an open-ended distribution rules out range and standard deviation alike, leaving quartile deviation as the practical choice. Where the extreme observations are known to be unreliable, the same reasoning applies.
- What the purpose demands — a rough indication of spread, wanted quickly, is served by the range. Any measure meant to represent the series properly must be built from all the observations, which narrows the choice to mean deviation and standard deviation.
- Whether a comparison is intended — one series is described by an absolute measure. Two series measured in different units, or with very different averages, must be compared by a relative measure, and the coefficient of variation is the one ordinarily used.
The four measures and their relative counterparts are collected in Table 19.15.
19.9 Summary
- A measure of central value tells us where a series centres, but nothing about how closely the observations gather around that centre. Two series may share an average and still differ entirely in their spread, which is why dispersion must be measured alongside the average.
- Dispersion is the extent to which the values of a series are scattered about an average of the series, or differ among themselves. It is measured to judge how far the average may be trusted, to describe the composition of a series, to compare two series, and to control variation where variation is undesirable.
- A good measure of dispersion should be rigidly defined, easy to understand and calculate, based on all the observations, unaffected by extreme values, stable across samples, and capable of algebraic treatment. No single measure satisfies all six conditions.
- Measures of dispersion are of two kinds.
- An absolute measure states the scatter in the original units of the data, and is used to describe a single series.
- A relative measure, or coefficient of dispersion, is an absolute measure divided by an average of the same series. It is a pure number and is used to compare two or more series.
- The absolute measures divide again by method. Range and quartile deviation are distance measures, taking the gap between two values. Mean deviation and standard deviation are average deviation measures, averaging the distances of all the observations from an average.
- Range is the difference between the highest and lowest value observed, \(R = H - L\), where \(H\) is the highest and \(L\) the lowest value. Its relative measure is the coefficient of range, \(\dfrac{H - L}{H + L}\), a pure number lying between 0 and 1.
- In a continuous series two methods are accepted — the difference of the mid-values of the highest and lowest classes, and the difference of the upper boundary of the highest class and the lower boundary of the lowest. The second always exceeds the first by one class width, so the method used must be stated.
- Range is simple and useful where the outer limits matter, but it rests on two values only, is dominated by extreme observations, and cannot be computed for an open-ended distribution.
- Quartiles divide an ordered series into four equal parts. Quartile deviation is half the distance between the upper and lower quartiles, \(QD = \dfrac{Q_3 - Q_1}{2}\), where \(Q_3\) and \(Q_1\) are the upper and lower quartiles; the undivided difference \(Q_3 - Q_1\) is the interquartile range. Its coefficient is \(\dfrac{Q_3 - Q_1}{Q_3 + Q_1}\).
- In individual and discrete series the quartiles stand at the \(\left(\dfrac{N+1}{4}\right)\)th and \(\dfrac{3(N+1)}{4}\)th items, where \(N\) is the number of observations or the total frequency.
- In a continuous series they are found by interpolation, \(Q_1 = l_1 + \dfrac{\dfrac{N}{4} - c.f.}{f} \times C\) and \(Q_3 = l_1 + \dfrac{\dfrac{3N}{4} - c.f.}{f} \times C\), where \(l_1\) is the lower limit of the quartile class, \(c.f.\) the cumulative frequency of the class before it, \(f\) its frequency and \(C\) its size.
- Quartile deviation ignores the outer quarters of the data, so it is unaffected by extreme values and can be computed for open-ended distributions, but it still rests on two values only.
- The deviations from the arithmetic mean always sum to zero, so their signs must be removed before they can be averaged. Mean deviation removes them by ignoring them; standard deviation removes them by squaring.
- Mean deviation is the arithmetic average of the absolute deviations of the observations from the mean or the median, \(MD_{\bar{x}} = \dfrac{\Sigma f|X - \bar{x}|}{\Sigma f}\) and \(MD_{m} = \dfrac{\Sigma f|X - M|}{\Sigma f}\), where \(X\) is an observation, \(f\) its frequency, \(\bar{x}\) the arithmetic mean and \(M\) the median. In an individual series the frequencies drop out and the divisor is \(N\).
- Its coefficient is the mean deviation divided by the same average it was taken from — \(\dfrac{MD_{\bar{x}}}{\bar{x}}\) or \(\dfrac{MD_{m}}{M}\).
- The mean deviation about the median is always the smaller of the two, since the median makes the total of the absolute deviations as small as it can be.
- It uses every observation, but ignoring signs is not a sound algebraic operation, and the measure leads no further.
- Standard deviation is the square root of the arithmetic mean of the squared deviations from the arithmetic mean, and is written \(\sigma\). It is computed from the arithmetic mean alone.
- Direct method — \(\sigma = \sqrt{\dfrac{\Sigma f x^2}{N}}\), where \(x = X - \bar{x}\) is the deviation from the actual mean and \(N\) the number of observations or the total frequency.
- Short-cut method — \(\sigma = \sqrt{\dfrac{\Sigma f d^2}{N} - \left(\dfrac{\Sigma f d}{N}\right)^2}\), where \(d = X - A\) is the deviation from an assumed mean \(A\), the subtracted term correcting for the gap between \(A\) and the true mean.
- Step deviation method — \(\sigma = \sqrt{\dfrac{\Sigma f d'^2}{N} - \left(\dfrac{\Sigma f d'}{N}\right)^2} \times C\), where \(d' = \dfrac{m - A}{C}\), \(m\) is the mid-value of a class and \(C\) the common class size. The final multiplication by \(C\) restores the answer to the unit of the data.
- All three methods give the same answer for the same data, and the choice of assumed mean never affects the result.
- The coefficient of standard deviation is \(\dfrac{\sigma}{\bar{x}}\). Expressed as a percentage, the same ratio is the coefficient of variation, \(CV = \dfrac{\sigma}{\bar{x}} \times 100\), where \(\sigma\) is the standard deviation and \(\bar{x}\) the arithmetic mean. A higher coefficient of variation means greater variability and therefore less consistency, and the comparison holds even between series measured in different units.
- Standard deviation is rigidly defined, based on all the observations and capable of algebraic treatment, which makes it the measure ordinarily used and the foundation of correlation, regression and sampling theory. Its demerits are that it is laborious to compute and that squaring gives extreme observations disproportionate weight.
- The choice of measure turns on what the data allow, what the purpose demands, and whether a comparison is intended. Open-ended classes or unreliable extremes point to quartile deviation; a quick rough answer point to range; a properly representative figure points to standard deviation; and a comparison across units or averages requires the coefficient of variation.
19.10 Points to Ponder
- An economy reports a rising average income year after year, while the dispersion of incomes widens at the same time. Has that economy improved? What would you need to know before answering, and which of the two figures would you put first in a report?
- Standard deviation squares the deviations, so an observation lying far from the mean counts for much more than one lying close to it. Where variation stands for risk — in the price of a share, or in the yield of a crop — is that extra weight a defect of the measure or exactly what is wanted?
- Quartile deviation sets aside the highest and lowest quarters of the data before measuring anything. When is discarding observations a sound response to unreliable extremes, and when is it a convenient way of removing the very cases a study ought to be about?
- Two workers are compared. One has the smaller standard deviation, the other the smaller coefficient of variation. If a firm must promote one of them for consistency, which figure should decide, and does the answer change if the two work in different departments producing different things?
- Suppose the wages in a firm had zero dispersion, every worker earning exactly the average. Would that be a desirable state of affairs, and what would it imply about how the firm rewards effort, skill and experience?
- Range is the least satisfactory measure by almost every property listed in this chapter, yet it is the one most often quoted in newspapers, market reports and weather bulletins. Why do simple measures survive their own defects, and what does the public use of a measure tell us that its statistical properties do not?
19.11 Objective Questions
- Which of the following measures of dispersion is not affected by the extreme values of a series? [1]
- Range
- Quartile deviation
- Standard deviation
- Coefficient of variation
- Assertion (A): The coefficient of variation is a pure number carrying no unit. Reason (R): It is obtained by dividing the standard deviation of a series by its arithmetic mean, so the unit of the data cancels. [1]
- Both A and R are true and R is the correct explanation of A.
- Both A and R are true but R is not the correct explanation of A.
- A is true but R is false.
- A is false but R is true.
- Fill in the blank: The difference between the upper quartile and the lower quartile of a series is called the ______. [1]
- State whether the following statement is true or false: Two series having the same standard deviation must also have the same coefficient of variation. [1]
- Match the measure in Column I with its description in Column II. [1]
| Column I | Column II |
|---|---|
| a. Quartile deviation | i. \(\dfrac{\sigma}{\bar{x}} \times 100\) |
| b. Coefficient of variation | ii. Also called the semi-interquartile range |
| c. Step deviation method | iii. Used to find the standard deviation of a continuous series with equal class intervals |
19.12 Check Your Concepts
- State any two differences between an absolute measure and a relative measure of dispersion. [2]
- The marks obtained by five students in a test are 12, 15, 18, 21 and 24. Calculate the range and the coefficient of range. [3]
- The daily wages of five workers, in hundreds of rupees, are 25, 30, 35, 40 and 45. Calculate the standard deviation by the direct method and the coefficient of variation. [4]
- The monthly savings of fifty households, in hundreds of rupees, are distributed as follows: 0–10, five households; 10–20, ten households; 20–30, twenty households; 30–40, ten households; 40–50, five households. Estimate the quartile deviation and its coefficient. [6]
19.13 Case-Based Question
- Ravi Malhotra runs a small garment unit and buys yarn from two suppliers. Over the past year, Sunrise Traders has taken an average of 12 days to deliver an order, with a standard deviation of 3 days. Deccan Yarns has taken an average of 20 days, with a standard deviation of 4 days. Ravi is inclined to call Sunrise Traders the steadier supplier because its deliveries vary by fewer days.
- Calculate the coefficient of variation of delivery time for each supplier. [2]
- State which supplier is the more consistent, and explain why a comparison of the two standard deviations alone would have misled Ravi. [2]