Why Volatility Scales with the Square Root of Time
Summary
The document explains why the square root of time relationship appears in volatility calculations. For processes with independent increments, the variance over a combined interval equals the sum of the variances over its subintervals. If the process is also homogeneous over time, so its parameters remain constant, variance grows in proportion to elapsed time and standard deviation grows with the square root of elapsed time.
It illustrates the argument for logarithmic returns in Levy models: the cumulant generating function scales linearly with time, so each cumulant, including the variance, also scales linearly. Geometric Brownian motion is given as a familiar example, with log-return variance proportional to time. The rule depends on the assumptions of independent increments and stable process parameters; changing volatility or dependence can make the scaling unsuitable as a forecast. The document gives a model-based explanation, not empirical evidence that the rule fits market returns in all settings.
Key ideas
- Independent increments make interval variances additive.
- With time-homogeneous parameters, variance grows linearly with the length of the interval.
- Standard deviation therefore scales with the square root of time under these assumptions.
- Levy processes and geometric Brownian motion illustrate the relationship for log returns.
- Changing parameters or dependent increments can undermine the square root scaling.
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# Mathematical underpinnings of the square root of time rule
# Mathematical underpinnings of the square root of time rule
Often when I am reading about options pricing (and/or options greeks) the square root of time continually comes up. What the mathematical justification for why this keeps on turning up?
## Answer by Alex C (score 9, accepted)
https://quant.stackexchange.com/a/30196
For any process with independent increments, by the very fact of statistical independence the variance of $x_{t3}-x_{t1}$ is going to be the sum of the variances of $x_{t2}-x_{t1}$ and $x_{t3}-x_{t2}$ for $t1\leq t2 \leq t3$. Many processes have independent increments, including ABM, GBM, Poisson, etc. Then if you add a homogeneity assumption (the parameters of the process do not change over time) you get a proportionality of the variance to the length of the time interval and thus a proportionality of the standard deviation to $\sqrt t$.
## Answer by LocalVolatility (score 2)
https://quant.stackexchange.com/a/30194
The reason is that in many common models including geometric Brownian motion, the variance of the logarithmic returns is proportional to time. Thus, their standard deviation/volatility is proportional to the square root of time.
Consider for example the class of Levy models where $X$ is is the logarithmic stock price process such that $S_t = S_0 e^{X_t}$. The cumulant generating function of $X_t$ takes the form
\begin{equation} \psi_{X_t}(\omega) = \psi_{X_1}(\omega) t, \end{equation}
where $\psi_{X_1}(\omega)$ is the characteristic exponent which is independent of $t$. You obtain the $n$-th cumulant as the $n$-th derivative of the cumulant generating function with respect to the transform parameter evaluated at zero, i.e.
\begin{equation} c_n(X_t) = \frac{1}{\mathrm{i}^n} \frac{\partial^n \psi_{X_t}}{\partial \omega^n}(0). \end{equation}
You immediately see that the cumulants are proportional to $t$. Since the second cumulant corresponds to the variance, this confirms that the standard deviation of logarithmic returns is proportional to the square root of time.
As mentioned the above setup includes the geometric Brownian motion setting with
\begin{equation} \psi_{X_t}(\omega) = \left( \mathrm{i} \omega \left( r - \frac{1}{2} \sigma^2 \right) - \frac{1}{2} \sigma^2 \omega^2 \right) t. \end{equation}
You get
\begin{equation} c_2 \left( X_t \right) = \sigma^2 t \end{equation}
as expected.Shown in full with attribution under the source's licence. Licence: CC BY-SA 4.0 (Stack Exchange)
This summary was written by Stratmill's research agent from the original; it is not a copy of the source.