Returns and volatility
The lesson "Interest, compounding and discounting" dealt with money that grows at a known rate. A stock does not: its price moves up and down in a way nobody can predict exactly. This lesson introduces the two numbers used to describe such movements, the average return and the volatility, and shows how both scale with the length of the holding period.
Prices and returns
Write for the price of a stock at time . Prices themselves are awkward to compare: a move of 5 means a lot for a stock at 20 and little for a stock at 1000. What an investor cares about is the change relative to the starting price. So instead of prices we study returns, the relative change over a period.
Throughout this lesson the stock pays no dividends, so the price change is the whole return.
Simple returns
The simple return from time to is
It is the number most people mean by "the stock went up 10%". Its drawback appears when periods are chained. Over two periods the total growth factor is the product , not the sum of the returns.
Example: a price goes from 100 to 110 and then back to 99. The simple returns are and . They add up to zero, yet the investor has lost 1%, because .
Log returns
The log return (continuously compounded return) is the natural logarithm of the growth factor:
It is the rate that, compounded continuously over the period, turns into , exactly as in "Interest, compounding and discounting": . Because a logarithm turns products into sums, log returns over consecutive periods add up:
In the example above, and . Their sum is , which correctly reports the 1% loss. For small moves the two kinds of return are nearly equal, since when is close to zero.
From here on, "return" means log return. Additivity is what makes the scaling rules below so simple.
Mean and standard deviation
Treat the return over one period as a random variable . Its mean (expected value) is the average return you would see over many repetitions. Its standard deviation measures the typical size of the deviation from that mean:
From a sample of observed returns we estimate them by
Example: four daily returns of , , and . The mean is . The deviations are , , and (in percent), their squares add up to 17, and per day.
Volatility
Volatility is the standard deviation of log returns, quoted per year. A stock with has annual log returns that typically land within about 20 percentage points of their mean. Volatility measures how uncertain the outcome is, not which direction it takes.
Volatility is the annualised standard deviation of log returns. The drift is the annualised mean log return.
Annualising and the square-root-of-time rule
Returns are measured daily or monthly, but and are quoted per year. To convert, make two assumptions: returns over non-overlapping periods are independent, and they all have the same distribution. Split a horizon of years into periods of length , each with mean and variance . The total log return is the sum of the period returns, so
The variance adds because the returns are independent. Taking the square root gives the square-root-of-time rule:
The mean grows in proportion to , the standard deviation only in proportion to . With about 252 trading days a year, a daily standard deviation of corresponds to an annual volatility of . In the other direction, per year means per month.
The normal distribution as a first model
A simple first model assumes that the log return over years is normally distributed:
This is natural given the previous section: the total log return is a sum of many small independent pieces, and such sums are approximately normal (central limit theorem). For a normal variable about 68% of outcomes fall within one standard deviation of the mean and about 95% within two.
Example: with , and years, the mean log return is and the standard deviation is . The one-standard-deviation range is to . In price terms, a stock starting at 100 ends between about and in roughly two cases out of three.
Real returns have fatter tails than the normal distribution: large moves happen more often than it predicts. The model is still the standard starting point, and later lessons build on it.
The figure plots the expected cumulative log return over horizons up to 10 years, with bands at and . Increase and note that the bands widen while the centre line does not move. Over short horizons the bands dominate the drift; only over long horizons does the line pull away from zero relative to their width.
- T = 1 y
- 6.0% ± 20.0%
- T = 4 y
- 24.0% ± 40.0%
- T = 9 y
- 54.0% ± 60.0%
Summary
- Returns, not prices, are the objects to model. Log returns add up over consecutive periods.
- Volatility is the annualised standard deviation of log returns; is their annualised mean.
- With independent, identically distributed returns, the mean grows like and the standard deviation like .
- A first model takes to be normal with mean and variance .
The next lesson, "Diversification and correlation", combines several assets and shows how their volatilities add up. Where the comes from is shown in "Random walks and Brownian motion", the first lesson of the Stochastic models track.