Brownian motion is nowhere differentiable. Its total variation is almost surely infinite. Classical
Riemann–Stieltjes integration requires the integrator to have bounded variation. How, then, can we
define ∫0THtdWt in a way that is mathematically precise and financially meaningful?
The Itô integral is the central technical object of stochastic calculus. Chapter 1 built Brownian motion and established its quadratic variation property [W]T=T. This chapter uses that property as a foundation. The strategy is:
Observe that pathwise Riemann–Stieltjes integration fails.
Define the integral for a small, explicitly computable class (simple processes).
Prove an isometry that makes the integral a bounded linear map in L2.
Extend to the full L2 class by density and closure.
The construction mirrors the standard L2 completion in functional analysis, and the isometry is its counterpart of Parseval's theorem.
Let f:[0,T]→R be a continuous function and g:[0,T]→R be the integrator. The Riemann–Stieltjes integral ∫0Tfdg exists whenever f is continuous and g has bounded variation:
∥g∥TV=Πsupk∑∣g(tk+1)−g(tk)∣<∞.
For Brownian motion, the opposite holds.
Brownian motion has infinite total variation
Almost surely,
k=0∑n−1∣Wtk+1−Wtk∣→∞
as the mesh ∣Π∣→0.
Proof
On a uniform partition with tk=kT/n, the increments are i.i.d.\ N(0,T/n).
Therefore
By the law of large numbers applied to the i.i.d.\ terms ∣Wtk+1−Wtk∣, the sum converges almost surely to ∞.
So Brownian paths are nowhere near having bounded variation. No classical integral theory applies directly.
Why infinite variation but finite quadratic variation?
Total variation sums ∣ΔW∣. Quadratic variation sums (ΔW)2. Because ΔW∼Δt, we have
∣ΔW∣∼Δt,(ΔW)2∼Δt.
Summing over n=T/Δt terms:
∑∣ΔW∣∼nΔt=T/Δt→∞,∑(ΔW)2∼n⋅Δt=T.
Quadratic variation lives in the right scaling window to remain finite. This is why (dW)2=dt is the key equation, and why the natural Hilbert space for stochastic integration is built on the L2 norm.
A process H=(Ht)0≤t≤T is called simple (or elementary) if there exists a partition 0=t0<t1<⋯<tn=T and Ftk-measurable random variables Hk satisfying E[Hk2]<∞, such that
Ht=k=0∑n−1Hk1(tk,tk+1](t).
The requirement that Hk is Ftk-measurable is the adaptedness condition: the value of the integrand at time tk may only use information up to tk.
Adaptedness is not optional
If Hk were allowed to depend on Wtk+1 — the future increment — the resulting integral would not be a martingale, and the isometry below would fail. In finance, this corresponds to using future prices to choose a present position: pure look-ahead bias.
For a simple process, we define the Itô integral as the finite sum
I(H)=∫0THtdWt:=k=0∑n−1Hk(Wtk+1−Wtk).
Each term is a product of a Ftk-measurable random variable with an independent increment. This is a finite sum of square-integrable random variables, so I(H)∈L2(Ω).
Since L2(Ω) is complete, the limit exists and is independent of the approximating sequence.
Itô integral as a left-endpoint Riemann sum over Brownian motion
Itô sum (left endpoint)0.8162
Stratonovich sum (midpoint)1.2593
Itô formula: ½(W₁² − 1)0.7593
Blue rectangles use H(t_k) — left endpoint, Itô convention. The Itô sum converges to ½(W₁² − 1), not ½W₁², because (dW)² = dt contributes an extra −½ correction — the Itô correction term. The Stratonovich midpoint sum converges to ½W₁².
The process (Mt)0≤t≤T is a martingale with respect to the filtration (Ft).
Proof sketch for simple processes
For s<t and a simple process adapted to a partition that includes s,
Mt−Ms=tk∈[s,t)∑HkΔWk.
Each term HkΔWk has mean zero conditionally on Fs (since Hk is Ftk⊇Fs-measurable and ΔWk is independent of Ftk with mean zero). Therefore
E[Mt−Ms∣Fs]=0,soE[Mt∣Fs]=Ms.
Trading P&L is a martingale under no-arbitrage
If Ht is the number of shares of a zero-drift asset held at time t, and the asset price satisfies
dSt=σtdWt (a pure diffusion under the risk-neutral measure), then the portfolio value
Pt=P0+∫0tHsdSs=P0+∫0tHsσsdWs
is a martingale. The expected P&L is zero: there is no predictable profit without risk. This is the
mathematical content of no-arbitrage in diffusion models.
The approximation uses (dW)2=dt in the same sense as the quadratic variation of Brownian motion.
Volatility as accumulated integrand squared
The quadratic variation [M]t=∫0tHs2ds is the accumulated squared magnitude of the integrand. In finance, if Ht is the dollar amount in the risky asset and dS/S=σdW, then the portfolio quadratic variation is ∫0tHs2σs2ds — the accumulated squared dollar-volatility exposure.
The two integrals are related by the correction formula
∫0THt∘dWt=∫0THtdWt+21[H,W]T,
where [H,W]T=∫0TdHsdWs is the cross-variation.
For a smooth function f applied to Brownian motion, Ht=f(Wt), one computes
[f(W),W]T=∫0Tf′(Ws)ds,
so the Stratonovich integral satisfies the classical chain rule: ∫f′(Wt)∘dWt=f(WT)−f(W0). The Itô integral instead satisfies the modified Itô formula in Chapter 3.
Which integral to use?
Itô: natural in finance (adapted integrands, no future look-ahead, martingale property), but its calculus has second-order correction terms.
Stratonovich: natural in physics/geometry (satisfies classical chain rule, coordinate-invariant under manifold transformations), but uses anticipating information.
The correction −2T is the signature of Itô calculus. Classical calculus would give ∫0Txdx=21x20T=21T for x=T, but that is the wrong analogy. The Itô integral of Wt against dWt is not 21T; it is the random variable 21WT2−21T.
The next chapter derives Itô's formula, the chain rule of stochastic calculus. Itô's formula is what makes the integral computable and connects it to classical analysis and partial differential equations.