Basic Prerequisites: 01 · From Zero and Stochastic Calculus & Itô’s Lemma.


1. Intuition & Practical Objective

Fractional Brownian motion is the mathematical object behind “rough vol”. This page derives the facts from first principles - the covariance, the stationary-increment variance , the self-similarity, and the Bergomi–Guyon skew functional - so that the rBergomi model of 02 · The rBergomi Model rests on proved identities rather than asserted ones.

The practical objective: derive from the covariance, understand why is Brownian and is rough (fractal dimension ), and derive the double integral that produces the power-law skew .


2. Mathematical Ground Truth & Derivations

2.1 Definition and covariance

fBm is the Gaussian, self-similar process with stationary increments whose autocovariance is (Mandelbrot–Van Ness 1968)

Stationary increments mean ; self-similarity means . From the covariance,

which is the exact scaling law that GJR estimate on log-volatility as .

2.2 Hurst and the two regimes

Hincrementsautocorrelationcharacter
anti-persistent (negatively correlated)rough - fractal dimension ; vol clustering via reversal
independent (BM)smooth Markovian baseline
persistent (positively correlated)long-memory / slowly-mean-reverting

The lag-1 autocorrelation follows directly: with , where (verified numerically in 01 · From Zero §3).

2.3 Self-similarity and the “one day ≈ one decade” scaling

Self-similarity has a striking consequence (GJR §3.4): over an observation scale , the rescaled vol process has the law of geometric fBm with vol . Since grows slowly for small , the law of log-volatility is nearly scale-invariant: between one day and five years ( days), - the vol coefficient barely changes. “Volatility over one day resembles volatility over a decade.” This is why a single roughness parameter captures behaviour across all horizons.

2.4 The Bergomi–Guyon skew functional (the bridge to prices)

For a forward-variance model the order-1 ATMF skew is (Bergomi ch 8, 04 · SV Dynamics)

For a power-law covariance kernel (the rBergomi kernel) the inner double integral is computable in closed form:

so . This is the derivation of the rough-vol skew power law - one boxed integral, no numerics needed, verified to 5 digits in 02 · The rBergomi Model §3.

2.5 Hurst estimation via the variogram

Because , an OLS regression of on - where is the sample mean-squared increment of log-vol - has slope . GJR’s estimate on SPX comes from exactly this variogram. The estimator is verified end-to-end (simulate fBm, recover H) in 04 · Hurst Estimation & Simulation.


3. Computational Implementation - exact fBm simulation and the Hurst recovery

We simulate exact fBm increments via the Hosking/Levinson recursion (O(n²), stdlib) - no approximate schemes - and verify (i) the increment variance law and (ii) that the variogram OLS recovers . Stdlib only.

Reading the output.

  • (i) The stationary-increment law is exact. equals to within over four decades of lag - the precise scaling GJR observe on log-volatility as . (The small drift at the largest lags is finite-sample boundary bias, not model error.)
  • (ii) The variogram is an unbiased, accurate H estimator. Simulating exact fBm at and running the variogram OLS recovers ; ; . This is the same estimator GJR apply to real log-vol - so when a paper reports , this is the mechanism behind the number.

4. Failure Modes & First-Principles Breakdowns

  1. The covariance formula assumes with the given normalisation. Shifting/scaling arguments are fine (self-similarity), but the form only holds with ; a two-sided fBm on needs the symmetric form with possibly negative - use the right domain.
  2. Hosking/Levinson drifts if the covariance matrix is nearly singular. For very close to or the Toeplitz matrix becomes ill-conditioned; clamp the innovation variance (as here) or the recursion produces negative variances (see §3’s max(...,1e-12)). For exactly use plain BM - don’t push fBm through the singular limit.
  3. The double integral needs . The inner converges only for , i.e. . The rough-vol range is fine, but the closed form is invalid at (a pole).
  4. Estimating H from the increments instead of the path. The variogram must be computed on (stationary increments, ), not on the second difference / increments-of-increments - a common slip that yields a spurious slope. And do not mistake the increment autocorrelation for long memory.

5. References

  • Mandelbrot & Van Ness (1968), Fractional Brownian motions, fractional noises and applications, SIAM Review 10(4), 422–437
  • Gatheral, Jaisson & Rosenbaum (2018), Volatility is rough, Quantitative Finance 18(6), 933–949
  • Hosking (1984), Modeling persistence in hydrological time series using fractional differencing / McLeod & Hipel
  • Bergomi (2016), Stochastic Volatility Modeling, ch 7–8
  • Bayer, Friz & Gatheral (2016), Pricing under rough volatility, Quantitative Finance 16(6), 887–904

6. Connected Graph Bridges