Convert a monthly Sharpe ratio to a longer additive horizon with serial covariance, and distinguish the population identity from HAC inference and compounding.
Autocorrelation adjusted Sharpe ratio
An autocorrelation adjusted Sharpe ratio converts a one-period Sharpe ratio to a longer horizon while including covariance between returns at different dates. It matters when comparing strategies whose monthly returns have different serial dependence: multiplying both monthly ratios by 12 can distort their annual-scale comparison.
Here, “adjusted” means Lo's time-aggregation correction for a sum of excess returns. It does not mean that the estimate has been corrected for every source of backtest bias or that its statistical significance is known. Lo (2002), Time Aggregation, equations 19–20.
Count the covariance pairs
Let xt=Rt−Rf,t be monthly excess return, subtracting the matching monthly cash return observation by observation. Assume covariance stationarity: a constant mean μ, a finite constant variance σ2>0, and lag-k covariance γk that depends on the lag rather than the calendar date. Define
ρk=σ2γk,SR1=σμ,Xq=j=1∑qxj.
The autocorrelation ρk measures correlation between observations k periods apart. The variance of the sum is an exact population identity:
There are q−k distinct pairs k months apart. Each appears twice in the double sum, once in each order. For a twelve-month sum, that means eleven lag-one pairs, ten lag-two pairs, down to one lag-eleven pair. The weights are consequences of this counting, not arbitrary choices about which lags seem important.
Since E[Xq]=qμ, the horizon Sharpe ratio is
SRq=Var(Xq)qμ=DqqSR1,Dq>0.
No normal-distribution assumption is needed for this identity. Zero autocovariance at every relevant lag gives Dq=1 and recovers square-root scaling; independence is sufficient but stronger than necessary. A zero horizon variance leaves the ratio undefined.
Take a hypothetical stationary population with SR1=0.10 and ρk=0.2k. This correlation pattern is consistent with a stationary AR(1) process; it is stipulated here, not estimated from a short return history. For q=12,
D12=1+2k=1∑11(1−12k)0.2k≈1.447917.
The sum's variance is about 17.375σ2, consisting of 12σ2 from individual months plus 5.375σ2 from covariance. Therefore,
Hypothetical stationary monthly population with Sharpe 0.10 and lag-k correlation 0.2 to the power k. Twelve-month sum variance is 17.375 monthly variance units, comprising 12 from variances and 5.375 from covariance. The adjusted horizon Sharpe is 0.288 versus naive 0.346.
Original analytical population example. Both comparisons hold the monthly mean and variance fixed; the horizon is an additive twelve-month excess-return sum.
Positive covariance makes the sum riskier than the zero-covariance calculation assumes. Negative covariance can offset risk: with the same monthly Sharpe and ρk=(−0.2)k, D12≈0.689815 and SR12≈0.417085.
The direction depends on the weighted sum of all relevant autocorrelations, not just ρ1. For positive monthly Sharpe, Dq>1 reduces the horizon ratio and 0<Dq<1 increases it. With negative monthly Sharpe, the same denominator adjustment moves the signed ratio in the opposite numerical direction: “positive dependence always lowers Sharpe” is too imprecise.
A horizon correction is not a confidence interval
In data, μ, σ and the autocorrelations are unknown. Plugging their estimates into the identity gives a horizon point estimate. Estimating eleven autocorrelations adds uncertainty; an apparent correction may itself be noisy. Fitting an AR(1) can reduce the number of parameters, but makes the geometric correlation pattern a modelling assumption. Lo (2002), The General Case and equations 23–26.
Heteroscedasticity and autocorrelation consistent (HAC) inference addresses a related, different question: how uncertain is an estimated mean or Sharpe ratio? For a stationary return series with summable autocovariances, the long-run variance is
Ω=γ0+2k=1∑∞γk.
Under suitable central-limit conditions, the variance of the estimated mean is approximately Ω/T, where T is the history's sample size. Newey–West estimates long-run covariance using tapered sample autocovariances and a bandwidth. Inference for a Sharpe ratio also needs the joint estimation uncertainty of its mean and variance; for the adjusted horizon ratio, the estimated lag covariances enter too. It is not enough to attach a mean's HAC standard error to the final ratio. Datta and Du (2012), sections 2 and 3.2.
Keep horizon q separate from sample size T and HAC bandwidth. The finite-horizon weights 1−k/q arise from the target sum. A HAC bandwidth controls estimation of a long-run object. Similar triangular weights do not make those objectives interchangeable. In this example, D12≈1.447917, while the infinite-horizon AR(1) variance ratio is (1+0.2)/(1−0.2)=1.5.
Compounding changes the target. A sum of simple excess returns is generally different from a portfolio's compounded return minus compounded cash return. Log returns add through time, but a Sharpe ratio defined on log returns is a different statistic. The formula above does not automatically deliver a compounded annual simple-return Sharpe. Sharpe's original discussion explicitly distinguishes summation, compounding and serial correlation. Sharpe (1994), Time Dependence.
Changing regimes change the inputs. A constant lag covariance is inappropriate when a strategy or return process changes materially. The general double-sum covariance identity still holds, but the stationary reduction to one γk per lag does not. An autocorrelation correction cannot make the history stationary.
Observed dependence still needs an explanation. Overlapping return windows or stale valuations can create dependence. Establish what each observation represents before interpreting the correction. The resulting ratio describes the recorded series; it does not independently recover unobserved economic returns, remove omitted costs, or adjust for selecting the best of many strategies.
Practice
Two consecutive monthly excess returns have the same population mean and variance, monthly Sharpe 0.20, and correlation −0.25. What is the Sharpe ratio of their sum, and why is 2(0.20) incorrect?
Answer. For two months, D2=1+2(1−1/2)(−0.25)=0.75. Hence SR2=2(0.20)/0.75≈0.326599, versus 0.282843 from square-root scaling. The negative covariance lowers the sum's variance to 1.5σ2 rather than 2σ2. No compounding is being performed.