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Two data sets can share a mean and be nothing alike. and both average 50, but one is tightly clustered and the other is not. A measure of captures the difference, and no summary of data is complete without one.
The big picture
Standard deviation is the measure that matters most, because it is the one the rest of statistics is built on. The normal distribution is defined by a mean and a standard deviation; hypothesis tests on a mean use it; standardising a value to a -score divides by it. The reason it wins over simpler alternatives is that it uses every data point while producing a number in the original units — the variance gets you there by squaring, and the square root brings you back. Understanding why those two steps exist stops the formula feeling arbitrary and makes the later work far easier.
What you'll be able to do
The is the largest value minus the smallest. It is trivial to compute and almost useless as a summary, because it depends on exactly the two most extreme values and ignores everything between them.
The (IQR) is , the spread of the middle half of the data. Because it discards the top and bottom quarters, an outlier cannot affect it — which pairs it naturally with the median.
For values, use position for and for with grouped data, interpolating within the class as you did for the median. The generalises this: the 10th to 90th percentile range, for instance, trims the extreme tenth from each end.
The range of 17 is dominated by the single value 20. The IQR of 7 describes where most of the data actually sits — the same contrast as mean versus median, for the same reason.
The natural idea is to average how far each value sits from the mean. But the deviations always sum to zero — that is what being the mean means — so their average is always zero and tells you nothing.
Squaring fixes it. Squared deviations are never negative, so they cannot cancel, and larger deviations are weighted more heavily. The mean of the squared deviations is the .
The cost is units: if the data is in metres, the variance is in square metres. Taking the square root gives the , back in the original units and therefore directly interpretable.
Taking absolute values instead of squaring would also stop the cancellation, and that statistic exists. Squaring is preferred because it is differentiable and behaves predictably under addition, which is what makes the whole theory of the normal distribution possible.
Computing every deviation is laborious. Expanding the definition gives an equivalent form that needs only two totals — the sum of the values and the sum of their squares.
For frequency data the same rearrangement applies with weighting each term. This is the version to use in practice, and the one the formula sheet provides.
Tip — "Mean of the squares minus the square of the mean" — in that order. Reversing it gives a negative number, which is impossible for a variance and is a useful self-check.
Under the coding , the standard deviation scales but does not shift: . The subtraction of slides every value along equally and so changes nothing about how spread out they are.
That asymmetry with the mean — which does shift — is examined directly, and it makes sense the moment you picture it: adding 10 to every value moves the whole distribution without stretching it.
When comparing two data sets, always compare location and spread together, and say what the comparison means in context rather than merely stating which number is bigger.
Tip — A comparison needs both measures and a context sentence: "Set B has a higher mean and a smaller standard deviation, so its scores are both higher and more consistent."
Think like an examiner
Common misconceptions
Spread
Stretch yourself
A frequency table gives , and . Find the mean and standard deviation. Then state what happens to each if every value is increased by 15.
Hint — Use the frequency forms. For the second part, think about whether a shift stretches the data.
Questions students ask
Key takeaways
How this fits the course
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