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"Frontmatter". In: Analysis of Financial Time Series

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RISKMETRICS 259we use log returns r t in data analysis. The VaR calculated from the quantile <strong>of</strong> thedistribution <strong>of</strong> r t+1 given information available at time t is therefore in percentage.The dollar amount <strong>of</strong> VaR is then the cash value <strong>of</strong> the financial position times theVaR <strong>of</strong> the log return series.Remark: VaR is a prediction concerning possible loss <strong>of</strong> a portfolio in a giventime horizon. It should be computed using the predictive distribution <strong>of</strong> future returns<strong>of</strong> the financial position. For example, the VaR for a 1-day horizon <strong>of</strong> a portfoliousing daily returns r t should be calculated using the predictive distribution <strong>of</strong> r t+1given information available at time t. From a statistical viewpoint, predictive distributiontakes into account the parameter uncertainty in a properly specified model.However, predictive distribution is hard to obtain, and most <strong>of</strong> the available methodsfor VaR calculation ignore the effects <strong>of</strong> parameter uncertainty.7.2 RISKMETRICSJ.P. Morgan developed the RiskMetrics TM methodology to VaR calculation; seeLongerstaey and More (1995). <strong>In</strong> its simple form, RiskMetrics assumes that thecontinuously compounded daily return <strong>of</strong> a portfolio follows a conditional normaldistribution. Denote the daily log return by r t and the information set available attime t −1byF t−1 . RiskMetrics assumes that r t | F t−1 ∼ N(µ t ,σt 2),whereµt is theconditional mean and σt2 is the conditional variance <strong>of</strong> r t . <strong>In</strong> addition, the methodassumes that the two quantities evolve over time according to the simple model:µ t = 0, σt 2 = ασt−1 2 + (1 − α)r t−1 2 , 1 >α>0. (7.2)Therefore, the method assumes that the logarithm <strong>of</strong> the daily price, p t = ln(P t ),<strong>of</strong> the portfolio satisfies the difference equation p t − p t−1 = a t ,wherea t = σ t ɛ tis an IGARCH(1, 1) process without a drift. The value <strong>of</strong> α is <strong>of</strong>ten in the interval(0.9, 1).A nice property <strong>of</strong> such a special random-walk IGARCH model is that the conditionaldistribution <strong>of</strong> a multiperiod return is easily available. Specifically, for ak-period horizon, the log return from time t + 1 to time t + k (inclusive) is r t [k] =r t+1 + ··· +r t+k−1 + r t+k . We use the square bracket [k] to denote a k-horizonreturn. Under the special IGARCH(1,1) model in Eq. (7.2), the conditional distributionr t [k] |F t is normal with mean zero and variance σt 2 [k], whereσ2t [k] can becomputed using the forecasting method discussed in Chapter 3. Using the independenceassumption <strong>of</strong> ɛ t and model (7.2), we haveσ 2t [k] =Var(r t[k] |F t ) =k∑Var(a t+i | F t ),where Var(a t+i | F t ) = E(σ 2t+i| F t ) can be obtained recursively. Using r t−1 =a t−1 = σ t−1 ɛ t−1 , we can rewrite the volatility equation <strong>of</strong> the IGARCH(1, 1) modeli=1

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