Itô's lemma
The lesson "Random walks and Brownian motion" showed that Brownian paths have no slope anywhere, so ordinary calculus does not apply to them directly. This lesson develops the replacement, Itô's lemma, the chain rule for functions of a random process. Its key ingredient is a surprising fact about squared increments of Brownian motion.
Increments in continuous time
Write for the increment of a Brownian motion over a short interval . From the definition of Brownian motion it is normal with mean zero and variance :
A process driven by Brownian motion is described by its increment too. The general Itô process has a drift and a volatility , which may depend on time and on the current value:
Read it as a recipe for one small step: a deterministic move plus a random move whose typical size is . For small the random part is much larger than the drift part, since is much larger than .
Quadratic variation
In ordinary calculus, squares of small increments are negligible: if is small, is much smaller and disappears in the limit. For Brownian motion this fails. Split into steps of length and add up the squared increments:
Each squared increment has mean , so for every . Each one also has variance (a property of the normal distribution), and the increments are independent, so
The sum keeps its mean while its randomness disappears: in the limit it equals exactly. This limit is the quadratic variation of Brownian motion. Example: on the standard deviation of is , which is for , for and for .
For a smooth path the same sum goes to zero, because each squared increment is of order . Brownian motion is rough enough that its squared increments add up to something finite.
The sum of the absolute increments behaves very differently. Each has mean , so on the total variation has mean : about for , for and for . It grows without bound. The length travelled by a Brownian path is infinite, yet the sum of its squared steps settles down to elapsed time.
The figure draws four Brownian paths on built from normal increments and plots the running sum of each against , together with the line . Switch between , and and press "New paths" a few times. The running sums hug the line more tightly as grows. The readouts, computed over 2000 paths at , show the mean of staying near 1, its standard deviation shrinking like , and the mean of growing like .
- Mean of Σ(ΔW)² at t = 1 (2000 paths)
- 1.000
- Std. dev. of Σ(ΔW)²
- 0.141 (√(2/n) = 0.141)
- Mean of Σ|ΔW|
- 7.98 (√(2n/π) = 7.98)
The result is written as a set of multiplication rules for small increments:
Quadratic variation: the squared increments of Brownian motion over add up to . In shorthand, .
Itô's lemma
Let be a smooth function and an Itô process as above. We want the increment of . Expand to second order in a Taylor series:
In ordinary calculus the third term would be dropped. Here it must be kept. Square using the multiplication rules: the and terms vanish and only survives:
Higher-order terms are of order or smaller and vanish. Substituting gives Itô's lemma:
Compared with the ordinary chain rule there is one extra drift term, . It is the price of the roughness of Brownian paths: the curvature of turns the random fluctuations of into a systematic drift of .
The square of Brownian motion
Take (so , ) and , with and . Itô's lemma gives
Ordinary calculus would give only . The random term has mean zero, so taking expectations of the accumulated increments leaves , which agrees with . Without the extra the expectation would wrongly stay at zero.
The logarithm of a stock price
The model of "Geometric Brownian motion" is , an Itô process with and . Apply Itô's lemma to , with and :
The right-hand side has constant coefficients, so it can be added up over directly:
This is the solution quoted in "Geometric Brownian motion", and the correction is exactly Itô's extra term. Naive calculus would have predicted a log drift of .
Example: , , . The log price drifts at per year, not . Over years the centre of the log price is , which corresponds to a median price of . The naive line would point to , which is the mean price, not where a typical path ends.
Size of the correction
Take one day, , with . The random part of the return, , is typically about . Its square is about , the same order of magnitude as the daily drift . Adding up such squares day after day does not average out, because they are never negative. That is why the second-order term changes the drift and cannot be ignored.
Summary
- An Itô process moves by : a drift step plus a random step of size about .
- Squared Brownian increments add up to elapsed time: , while and vanish.
- Itô's lemma: . The term is new compared with ordinary calculus.
- Applied to under GBM it gives .
The next lesson, "Change of measure and Girsanov's theorem", shows how the drift in this solution is replaced by for pricing; "Monte Carlo option pricing" then uses the resulting formula to draw terminal stock prices and estimate option prices by averaging.