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  • 8/9/2019 Steiner 12 Annualized Volatility

    1/8Electronic copy available at: http://ssrn.com/abstract=2007620

    2011, Andreas Steiner Consulting GmbH. All rights reserved. 1 / 8

    Research Note

    Andreas Steiner Consulting GmbH

    February 2012

    Annualized Volatility

    Introduction

    In this research note, we compare S&P 500 volatility figures calculated with the popular

    square-root-n rule to volatility figures derived from time-aggregated daily returns and try to

    reconcile the differences with popular time-series models featuring serial correlation inreturns or volatilities.

    We show that the deviations from the square-root-n rule cannot be explained with serial

    correlation in returns, rather with a GARCH model. We conclude that volatility figures

    annualized with the square-root-n rule should not be interpreted as accurate estimates for

    true annual volatility. The square-root-n rule is also not suitable to standardize volatility

    figures for reporting purposes.

    The Square-Root-N Rule

    Volatility is financial market lingo for standard deviation of continuous returns1 and

    generally used as a measure for return dispersion over time and a proxy for risk,

    respectively for uncertainty.

    If continuous returns are modeled as stochastic processes, volatility can be interpreted as

    one particular characteristic of the process. Justified by the idea that price changes are

    largely driven by unexpected changes in valuation factors, it is typically assumed that price

    changes2of financial assets are independent over time. In fact, this assumption is nothing

    else than assuming that markets exhibit weak-form information efficiency.

    It can be shown formally that this assumption leads to the so called square-root-n rule for

    annualizing volatilities3

    (1) nCalculatedAnnualized

    with Calculatedas the standard deviation measured from a time series of continuous returns

    and n being the data frequency of this time series expressed in periods per annum. For

    example, if we are calculating volatility of 6% from a monthly return time series, the square-

    root-n rule tells us that the annualized volatility is

    (2) %78.2012%6 Annualized

    http://www.andreassteiner.net/consulting/http://www.andreassteiner.net/consulting/
  • 8/9/2019 Steiner 12 Annualized Volatility

    2/8Electronic copy available at: http://ssrn.com/abstract=2007620

    2011, Andreas Steiner Consulting GmbH. All rights reserved. 2 / 8

    The assumptions underlying the rule imply that it should not make a difference whether we

    calculate annual volatility from annual, monthly, daily etc. returns. Therefore

    (3) 412250,,,

    QuarterlyCalculatedMonthlyCalculatedDailyCalculatedAnnualized

    More generally, the square-root-n rule can be used to convert volatilities calculated from

    returns with a certain frequency to volatility figures for returns over a longer time period. For

    example, quarterly volatility can be derived from monthly volatilities as follows

    (4) 3, MonthlyCalculatedQuarterly

    Ironically, the square-root-n rule is used every day by thousands of active investment

    managers in ex ante as well ex post portfolio analytics, i.e. investment managers which can

    only create value-added for their clients if markets are at least informationally inefficient of

    the weak form.

    Annualized S&P500 Volatilities

    In order to assess the validity of the square-root-n rule, we have analyzed a data set

    consisting of S&P 500 daily continuous price returns from January 5, 1987 to November 20,

    2011 (data source: Yahoo Finance).

    We calculate annualized S&P500 volatility figures with two methods

    Square-Root-N rule: Using daily volatility as a starting point, we calculate volatility

    figures for various longer time periods up to one year (250 trading days)

    Time-Aggregated Returns: Instead of converting volatilities, we convert the return

    data. For example, weekly continuous returns can be calculated from daily returns

    by simply adding five daily observations. The weekly return series generated this

    way can then be used to calculate weekly volatility.

    An alternative way to time-aggregated returns would be to resample/bootstrap from the

    daily return data set. Nave resampling procedures destroy any dependence of returns or

    volatilities over time. More sophisticated resampling procedures trying to preserve

    dependence patterns exist, but introduce additional assumptions into the analysis. As

    intertemporal dependence patterns are at the core of the issues discussed here, we prefer

    to calculate volatilities from historical time-aggregated returns as described above.

    The results from the above calculations4can be summarized graphically

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    0.00%

    2.50%

    5.00%

    7.50%

    10.00%

    12.50%

    15.00%

    17.50%

    20.00%

    22.50%

    25.00%

    0 50 100 150 200 250

    Annualized

    Volatility

    Time Period [Expressed in Number of Periods p.a.]

    Time-Aggregated Returns

    Square-Root-N Rule

    As we can see, volatilities calculated with the square-root-n rule generally do not coincide

    with true historical volatilities calculated from time-aggregated returns. In this particular

    case, the square-root-n rule seems to overestimate volatility on average by approximately

    15%, in some cases by almost 25%.

    The above result that returns are not independent is not really new, but has been reportedin numerous empirical studies. The more interesting question is: which kind of

    independence over time causes the square-root-n to fail? This question is of practical

    relevance, since certain dependence structures allow to filter the original data such that

    the square-root-n rule can still be used.

    Dependence in Returns and Volatilities

    The simplest way to model dependence of returns over time is to assume that returns are

    linearly autocorrelated5. Various explanations exist for autocorrelation in returns. For

    example, it is rather typical to find autocorrelation in returns on markets with pricing issues

    (e.g. fixed income, private equity, real estate).

    Autocorrelation patterns in returns can be detected in a chart plotting autocorrelation

    coefficients for returnsat various lags. For our S&P500 data

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    -8.00%

    -6.00%

    -4.00%

    -2.00%

    0.00%

    2.00%

    4.00%

    6.00%

    1 815

    22

    29

    36

    43

    50

    57

    64

    71

    78

    85

    92

    99

    106

    113

    120

    127

    134

    141

    148

    155

    162

    169

    176

    183

    190

    197

    204

    211

    218

    225

    232

    239

    246

    Autocorrelation

    Coefficient

    Lag

    The red dotted lines define a confidence band; autocorrelation coefficients outside the band

    can be considered statistically significant.

    As we can see, autocorrelation coefficients for daily S&P500 returns are generally small,

    and not statistically significant most of the time. This picture is rather typical for a rather

    efficient market; price changes seem to be unpredictable, unsuitable for simple shorts-term

    momentum or contrarian trading strategies.

    One popular method to remove autocorrelations is the Blundell-Ward filter. This filter iscapable of removing first-order autocorrelations (i.e. autocorrelations calculated at lag one).

    If we apply the Blundell-Ward filter to our S&P500 return series and then recalculate

    volatilities, we get

    0.00%

    2.50%

    5.00%

    7.50%

    10.00%

    12.50%

    15.00%

    17.50%

    20.00%

    22.50%

    25.00%

    0 50 100 150 200 250

    Annualized

    Volatilit

    y

    Time Period [Expressed in Number of Periods p.a.]

    Time-Aggregated Returns

    Square-Root-N Rule

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    As we can see, the Blundell-Ward filter removing first-order autocorrelations does not

    improve the performance of the square-root-n rule significantly. The square-root-n rule still

    systematically overestimates true volatilities.

    Interestingly, autocorrelations for the squared returns of the same return time series

    look very different

    -5.00%

    0.00%

    5.00%

    10.00%

    15.00%

    20.00%

    25.00%

    30.00%

    35.00%

    1 815

    22

    29

    36

    43

    50

    57

    64

    71

    78

    85

    92

    99

    106

    113

    120

    127

    134

    141

    148

    155

    162

    169

    17

    6

    183

    190

    197

    204

    211

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    239

    246

    Autocorrelatio

    n

    Coefficients

    Lags

    Autocorrelations in squared returns are clearly much larger (as high as 30%), statistically

    significant and exhibit a decaying pattern with lag size. This pattern is typical for first-order

    autoregressive processes. How do we interpret autocorrelations in squared returns

    economically? This can be seen from the definition of standard deviation if we assume that

    the arithmetic mean is so small that it can be neglected

    (5)

    N

    i

    ir

    N

    i

    i rN

    rrN 1

    2

    01

    2

    1

    1

    1

    1

    If the average return is small (and average daily returns are small indeed), then the

    squared return can be interpreted as a contribution to volatility, respectively a volatility

    innovation. Autocorrelations in squared returns can, therefore, be interpreted as

    autocorrelation in volatility.

    The most popular model exhibiting autocorrelation in volatility is GARCH(1,1), a specific

    parameterization of a more general class of generalized autoregressive conditional

    heteroscedastic models. Estimating the GARCH(1,1) allows one to compute short-term

    volatilities, which are assumed to exhibit first-order autocorrelation.

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    It looks like the GARCH(1,1) model explains autocorrelation in squared returns rather well.

    In the chart below, we applied the square-root-n rule and volatility calculations based on the

    time-aggregated returns to the GARCH(1,1)-standardized return

    -

    2.00

    4.00

    6.00

    8.00

    10.00

    12.00

    14.00

    16.00

    18.00

    20.00

    0 50 100 150 200 250

    Annualized

    Volatility

    Time Period [Expressed in Number of Periods p.a.]

    The GARCH(1,1) model nicely removes the systematic bias: the differences between the

    volatilities calculated from time-aggregated returns and with the square-root-n rule are notonly smaller, but their signs seem to vary randomly.

    Unfortunately, the volatility figures calculated from GARCH(1,1) standardized returns no

    longer have an economic meaning. This is not a surprise, because GARCH(1,1) not only

    feature first-order autocorrelation of volatilities, but also mean reversion. For example, in

    turbulent times with high realized volatilities, volatilities have a tendency to revert back to a

    lower long-term value. Annualizing with a square-root-n rule becomes meaningless, as we

    would either need to predict future volatility innovations or work with expected volatility

    innovations (which are zero by definition). Annualizing in a GARCH world is really

    calculating forward volatilities, given current volatility levels and some GARCH parameters.6

    Conclusions

    Unlike returns, true volatility is a characteristic of a financial asset or portfolio which

    cannot be measured directly, but always has to be estimated7. This statement applies to ex

    ante as well as ex post analysis. While ex post return measurement is mainly an

    accounting exercise, measuring ex post return volatility is about statistical inference,

    requiring a rather different skill set from the person executing the calculations.

    The square-root-n rule is a formula based on very specific assumptions. Unfortunately, the

    rule is used by many practitioners without questioning whether data characteristics justifythe underlying assumptions. Additionally, many systems used by practitioners do not

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    generate indicators which would allow users to assess the quality of the annualized

    volatility figures calculated.

    We do not recommend annualization of volatility figures for reporting purposes, as the

    operation is likely to introduce systematic biases when comparing results for different return

    time series. We recommend calculating annualized volatility from time-aggregated (i.e.annualized) returns instead. If the square-root-n rule has to be used, for example, due to

    lack of access to the return series, we recommend to disclose additional information like

    the data frequency at which the original volatility calculations were performed or statistical

    indicators for autocorrelation in returns.

    1See our research note on how to calculate discrete volatility.

    2And therefore returns, which are nothing else than relative price changes.

    3There exist other simple scaling rules if we make stronger assumptions about the stochastic

    process generating returns. For example, if we assume that returns follow a so-called stable

    distributions. But as financial returns generally exhibit finite variances, stable distributions are

    generally not relevant for financial time series.

    4All calculations in this research note were performed using our Advanced Portfolio Analytics

    Excel Add-In, seewww.andreassteiner.net/apalibfor more information.

    5Some authors use the expression serial correlation instead of autocorrelation.

    6The formulas to calculate expected forward volatiles can be found in the GARCH literature.

    7Alternatively, volatility can be inferred from markets: ex ante volatility is traded on rather liquid

    markets (e.g. VIX). Ex post volatility is traded on (rather illiquid) OTC markets for certain

    derivative instruments (e.g. variance swaps).

    http://www.andreassteiner.net/apalibhttp://www.andreassteiner.net/apalibhttp://www.andreassteiner.net/apalibhttp://www.andreassteiner.net/apalib