Combining and Propagating Uncertainties
You rarely measure the thing you actually want. You want a density, but you measure a
mass and a volume and divide. You want a speed, but you measure a distance and a time.
You want the strength of gravity g, but you measure a pendulum's length and
its swing time. In every case the final answer is calculated from measurements that each carry
their own little fog of uncertainty.
So a natural question: if each measurement is uncertain, how uncertain is the result you build from them?
The fog doesn't vanish when you press the buttons on a calculator — it propagates, flowing
through the arithmetic into the final number. This page gives you the small set of rules that tell you
exactly how much fog comes out the other end.
Two ways to state an uncertainty
Before combining anything, be fluent in the two languages of uncertainty — because the rules that follow
switch between them.
-
The absolute uncertainty is the raw \pm in the same units as
the quantity: a length of 12.4 \pm 0.2\,\text{cm} has an absolute uncertainty
of 0.2\,\text{cm}.
-
The percentage (fractional) uncertainty compares that \pm
with the size of the value itself:
\%\text{ uncertainty} = \dfrac{\text{absolute uncertainty}}{\text{value}}\times100.
So 12.4 \pm 0.2\,\text{cm} carries a percentage uncertainty of
\dfrac{0.2}{12.4}\times100 = 1.6\%. To go the other way — from a percentage back
to an absolute — just undo the division:
\text{absolute uncertainty} = \dfrac{\%\text{ uncertainty}}{100}\times\text{value}.
A resistor quoted as 470\,\Omega \pm 5\% therefore has an absolute uncertainty
of \dfrac{5}{100}\times 470 = 23.5\,\Omega, i.e.
470 \pm 23.5\,\Omega. Being able to slide between the two forms in your head is
the whole trick, because each combining rule wants one particular form.
Adding or subtracting: add the absolute uncertainties
When your result is a sum or a difference of measured quantities, the worst case is that
both errors push the same way, so their absolute uncertainties simply add:
Q = a \pm b \quad\Longrightarrow\quad \Delta Q = \Delta a + \Delta b.
Notice it is the same rule whether you add or subtract — subtracting doesn't subtract the
uncertainties, it still adds them. Uncertainty only ever grows.
Worked example — an extension. A spring's length is measured before and after loading:
L_1 = 45.0 \pm 0.5\,\text{mm} and
L_2 = 68.0 \pm 0.5\,\text{mm}. The extension is
e = L_2 - L_1.
- Best value: e = 68.0 - 45.0 = 23.0\,\text{mm}.
- Absolute uncertainty: \Delta e = \Delta L_2 + \Delta L_1 = 0.5 + 0.5 = 1.0\,\text{mm}.
- Result: e = 23.0 \pm 1.0\,\text{mm}, a percentage uncertainty of
\dfrac{1.0}{23.0}\times100 = 4.3\%.
Look what just happened to the percentages. Each length was only about
1\% uncertain, yet their difference is 4.3\% uncertain —
because subtracting two close numbers keeps the absolute \pm the same size while
shrinking the value. Hold that thought; it comes back in the Watch out! below.
Multiplying or dividing: add the percentage uncertainties
When your result is a product or a quotient, absolute uncertainties can't add — they're in
different units (you can't add grams to millilitres). What add instead are the percentage
uncertainties:
Q = \dfrac{a\,b}{c} \quad\Longrightarrow\quad \%\Delta Q = \%\Delta a + \%\Delta b + \%\Delta c.
Every factor on top or bottom contributes its percentage uncertainty, all added together — division counts
exactly the same as multiplication.
Worked example — a density. A metal block is measured as
m = 240 \pm 2\,\text{g} and
V = 30.0 \pm 0.6\,\text{cm}^3, and
\rho = \dfrac{m}{V}.
- Best value: \rho = \dfrac{240}{30.0} = 8.0\,\text{g/cm}^3.
- Percentage uncertainties of the inputs:
\%\Delta m = \dfrac{2}{240}\times100 = 0.83\% and
\%\Delta V = \dfrac{0.6}{30.0}\times100 = 2.0\%.
- Add them: \%\Delta \rho = 0.83\% + 2.0\% = 2.83\%.
- Convert back to absolute: \dfrac{2.83}{100}\times 8.0 = 0.23\,\text{g/cm}^3,
so \rho = 8.0 \pm 0.2\,\text{g/cm}^3 (uncertainty to 1 s.f.).
A second example — a speed. d = 100 \pm 1\,\text{m} (a
1\% track) covered in t = 20.0 \pm 0.4\,\text{s} (a
2\% timing). Then v = d/t = 5.0\,\text{m/s} with
\%\Delta v = 1\% + 2\% = 3\%, i.e.
5.0 \pm 0.15\,\text{m/s}. The routine is always the same: turn each input into a
percentage, add, then turn the total back into an absolute \pm if you need one.
Raising to a power: multiply the percentage by n
A power is just repeated multiplication, so raising a quantity to the power n
adds its percentage uncertainty to itself n times — which is the same as
multiplying it by n:
Q = a^{n} \quad\Longrightarrow\quad \%\Delta Q = n \times \%\Delta a.
Squaring doubles the percentage uncertainty; cubing trebles it. This works
for any real n, so a square root (n = \tfrac12)
halves it.
-
Area of a square. A side s is
1.5\% uncertain. Its area A = s^2 is
2 \times 1.5\% = 3.0\% uncertain.
-
Volume from a radius. For a sphere V = \tfrac{4}{3}\pi r^3. If
r is 2\% uncertain, then
\%\Delta V = 3 \times 2\% = 6\% — the constant
\tfrac{4}{3}\pi is exact and adds nothing.
Worked example — g from a pendulum. A pendulum of length
L and period T gives
g = \dfrac{4\pi^2 L}{T^2}. Suppose
\%\Delta L = 1\% and \%\Delta T = 0.5\%. Combining the
product/quotient rule with the power rule:
\%\Delta g = \%\Delta L + 2\,\%\Delta T = 1\% + 2 \times 0.5\% = 2\%.
The T^2 makes the timing count double — which is exactly why careful
experimenters time many swings at once to shrink \%\Delta T.
The rules for combining uncertainties
To propagate uncertainty through a calculation, match the operation to its rule:
-
Addition / subtraction Q = a \pm b: add the
absolute uncertainties, \Delta Q = \Delta a + \Delta b.
-
Multiplication / division Q = ab or
Q = a/b: add the percentage uncertainties,
\%\Delta Q = \%\Delta a + \%\Delta b.
-
Powers Q = a^n: multiply the percentage
uncertainty by n, \%\Delta Q = n\,\%\Delta a.
-
Exact constants (like 2,
\pi, \tfrac{4}{3}) carry no uncertainty and are
ignored.
See it: the biggest contributor wins
Here is the density calculation \rho = m/V as a picture. The top two bars are the
percentage uncertainties of your two measurements; the bottom bar is the combined percentage uncertainty of
the density — and it is exactly the two upper bars laid end to end, because for a quotient the percentages
add. Drag the sliders and watch which input pushes the total up hardest.
Hunt the dominant term
Because the percentage uncertainties simply add, the final uncertainty is bossed around by
whichever measurement has the biggest percentage uncertainty. In the density example the
volume (2.0\%) dwarfed the mass (0.83\%): halve the
volume's uncertainty and you barely-improve the mass, but you nearly halve the total.
This is the single most useful idea on the page. To improve an experiment, don't polish every measurement
equally — find the term with the largest percentage uncertainty and attack that one. Spending an
afternoon refining a measurement that already contributes 0.1\% while another
contributes 5\% is wasted effort.
The three slips that trip up almost everyone combining uncertainties:
-
Don't mix the two rules up. For + and
- you add the absolute uncertainties; for
\times and \div you add the percentage
uncertainties. Adding percentages in a subtraction, or absolutes in a division, is the classic exam-killer.
-
Subtracting two close values can blow up the percentage uncertainty. If
L_1 = 50.0 \pm 0.5 and L_2 = 51.0 \pm 0.5\,\text{mm},
the difference is 1.0 \pm 1.0\,\text{mm} — a 100% uncertainty!
The absolute \pm stayed the same, but the value collapsed. Avoid designing an
experiment around the tiny difference of two big numbers.
-
A squared quantity doubles the percentage uncertainty — don't forget the factor of
n. In g = 4\pi^2 L/T^2 the period enters as
T^2, so its \%\Delta T counts twice. Treating
T^2 like a plain factor quietly halves the timing's true contribution.
Every error bar you've ever drawn is a propagated uncertainty. Plotting
T^2 against L for that pendulum? The vertical bar on
each point is \%\Delta(T^2) = 2\,\%\Delta T converted back to an absolute
\pm in T^2; the horizontal bar is
\Delta L. The bars then set the honest range of gradients you could draw
through the data — a "steepest" and a "shallowest" line — and the spread of those gradients becomes the
uncertainty in your final answer for g.
This is why professional labs obsess over the single dominant term. When physicists announced the mass of
the Higgs boson, or when a company certifies a resistor to \pm 1\%, an enormous
amount of the work is exactly this bookkeeping: chasing down whichever measurement contributes the largest
percentage uncertainty and spending the budget there. Propagating uncertainties isn't busywork — it's how you
know whether your result means anything at all.