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No measurement is ever perfectly exact — every reading you take carries some , and every experiment has some kind of error built into it. A-Level physics doesn’t just want you to record a number; it wants you to say honestly how much you trust it, and to carry that honesty correctly through every calculation that number feeds into.
What you'll be able to do
A causes readings to scatter unpredictably above and below the true value — caused by things like reaction time in stopwatch timing, or reading a scale from a slightly different angle each time. Random errors can be reduced by taking repeated readings and averaging, since the scatter tends to cancel out.
A shifts every reading consistently in the same direction by roughly the same amount — for example a top-pan balance that hasn’t been zeroed, adding a fixed offset to every mass reading. Repeating the measurement does nothing to reduce a systematic error, because every repeat is shifted the same way; you can only remove it by finding its cause and correcting for it (or recalibrating the instrument).
Tip — Averaging more readings can only ever reduce random error. If your average value is consistently offset from the accepted value in one direction, suspect a systematic error, not insufficient repeats.
describes how close repeated measurements are to each other (small random error, but not necessarily close to the true value). describes how close a measurement is to the true, accepted value (small overall error, both random and systematic). It’s entirely possible to have precise but inaccurate readings — tightly clustered, but clustered around the wrong value because of a systematic error.
The of an instrument is the smallest change in the quantity it can detect — for a ruler with millimetre markings, the resolution is 1 mm. Resolution sets a lower limit on the uncertainty of any single reading: you cannot claim a smaller uncertainty than the instrument’s resolution allows.
Tip — Precise ≠ accurate. Picture a dartboard: all darts clustered tightly together but off to one side is precise but inaccurate; darts scattered widely but centred on the bullseye is accurate but imprecise.
The is the actual size of the possible error in a measurement, in the same units as the measurement itself (e.g. cm). The is the absolute uncertainty divided by the measured value (no units), and the is the fractional uncertainty expressed as a percentage.
Tip — A smaller percentage uncertainty always means a more precise measurement relative to its size — this is why percentage uncertainty, not absolute uncertainty, is the fair way to compare the quality of two very different measurements.
When quantities are , add their absolute uncertainties. When quantities are , add their percentage (or fractional) uncertainties. When a quantity is raised to a power , multiply its percentage uncertainty by .
Tip — Powers punish uncertainty: a cubic relationship like volume from radius triples the percentage uncertainty, so small measuring errors in a repeatedly-multiplied quantity balloon quickly.
When you take several repeated readings of the same quantity, a good working estimate of the uncertainty in their mean is half the : half the difference between the largest and smallest reading. This gives a simple, defensible uncertainty without needing formal statistics.
When a quantity is found from the gradient of a graph, uncertainty is estimated using the method: draw the best-fit line through the data, then the steepest and shallowest lines that still reasonably fit within the error bars on the data points. The uncertainty in the gradient is then half the difference between the best-fit gradient and the worst-fit gradient.
Tip — Always quote the absolute uncertainty to the same number of decimal places as the mean it belongs to — “2.01 ± 0.04 s”, never “2.01 ± 0.035729 s”.
Equation recap
Common mistakes to avoid
Key takeaways
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