The
Itô integral uses left-endpoint sampling, while the Stratonovich integral for continuous semimartingales can be defined using symmetric endpoint averages. For a scalar SDE with differentiable
diffusion coefficient b, a Stratonovich drift
a corresponds to the Itô drift
a+21bbx. The same process can be written in either convention after converting its drift.
For a financial
trading strategy, the natural sum multiplies the number of units held at the start of an interval by the price movement during that interval. This is the Itô convention. A symmetric approximation incorporates how the holding itself changed over the interval. If holding and price move together, their product leaves a correction. Stratonovich calculus incorporates that correction into the integral, which is why its
chain rule has the familiar ordinary-calculus form.
Write ΔWi=Wti+1−Wti and similarly for a continuous semimartingale H. The difference between the symmetric sum and the left-endpoint sum is
i∑(2Hti+Hti+1−Hti)ΔWi=21i∑ΔHiΔWi.
The limit is 21[H,W]T, so
∫0THt∘dWt=∫0THtdWt+21[H,W]T.
With Ht=b(t,Xt) and sufficient smoothness, the Brownian coefficient of H is bx(t,Xt)b(t,Xt). Its covariation with W integrates this coefficient over time. As a result,
dXt=a(t,Xt)dt+b(t,Xt)∘dWt=(a+21bbx)(t,Xt)dt+b(t,Xt)dWt.
To get the SDE correction, isolate the noise in
dHt for
Ht=b(t,Xt).
Itô's formula gives Brownian coefficient
bx(t,Xt)b(t,Xt) because the coefficient of
dWt in
dXt is
b. Time and drift terms contribute zero to the covariation with
W. This leaves
d[H,W]t=bxbdt, so the half-covariation in the integral becomes an ordinary drift adjustment. In particular, constant additive noise has
bx=0 and the two conventions give the same drift.
Take the Stratonovich equation dXt=σXt∘dWt with X0=x>0. Its chain rule gives dlogXt=σ∘dWt, and the integrand σ is constant. Therefore Xt=xeσWt. In Itô form, this same process has drift 21σ2Xt, which follows directly by applying Itô's lemma to the exponential.
Now take the Itô equation dYt=σYtdWt with the same initial value. Its solution is Yt=xeσWt−21σ2t. With x=100, σ=0.30 and t=1, the first process has mean 100e0.045≈104.60 and the second has mean 100. Setting the displayed drift coefficient to zero in each convention describes two different processes. For a constant diffusion coefficient, bx=0 and this drift adjustment vanishes.
One way to check the correction without solving an SDE is to set Ht=Wt. The symmetric sum telescopes because 21(Wti+Wti+1)ΔWi=21(Wti+12−Wti2). Thus the Stratonovich integral is WT2/2, while the Itô integral is (WT2−T)/2. The gap is exactly half of [W,W]T.
References and next steps