LECTURE 8 (pas le temps de niaiser !) Flashcards

1
Q

Why is the cst volatility hypothesis rejected by data ?

A

Volatility tend to cluser in time

Better to use conditional volatility since more relevant

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2
Q

What does volatility clustering suggest ?

A

Conditional return distribution is time-varying

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3
Q

Why is volatility a proxy for risk ?

A
  • Forecasting return
  • Pricing of derivative
  • Asset allocation
  • Risk mngmnt
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4
Q

What is volatility’s major problem ?

A

Not directly observable from returns

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5
Q

What is the unconditional volatility ?

A

sample std deviation

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6
Q

What are the several ways to measure volatility ?

A
  • Squared & absolute returns
  • Historical volatility
  • EWMA
  • RiskMetrics
  • Square Root of time rule
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7
Q

What is the problem with squared returns ?

A

Noisy volatility estimator since underestimates true values

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8
Q

What are absolute returns ?

A

εt ̴ N(0,σt^2) then E[|εt|] = σt 2√π

where σ’t = |εt|/2√π is a proxy of σt

Goes back to 0 = mkt closure

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9
Q

What is historical volatility ?

A
  • Very simple measure = moving avg
  • Problem : same weight to old & new information

• Drawback : generates pronounced ghost features
o After extreme event → huge increase in historical volatility stays as long as avging period

• Useful to measure LT volatility but not successful in ST

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10
Q

What is EWMA ?

A

• Overweights new information → weight drops over time : φ ϵ [0;1]
o σ^2(t) = φσ^2(t-1) + (1 – φ)(r(t-1) – μ’)^2

  • (1 – φ)(r(t-1) – μ’)^2 = measure of intensity of volatility‘s reaction to mkt event
  • φσ^2(t-1) = measure of persistence in volatility
  • Recommended value φ ϵ [0.75;0.98]
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11
Q

What is RiskMetrics ?

A
  • Special case of EWMA
  • Log-returns = conditionally normal
  • Daily volatility constructed assuming μ’=0 and φ=0.94
  • Same approach to produce forecasts of covariance
  • Allows estimation of large-dimensional covariance matrices
  • Use same φ so covariance matrix = semi-positive definite
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12
Q

What is the square root of time rule ?

A
  • Specific cases where possible to forecast variance for different horizon
  • If not serially correlated, V[rt(k)] = tσ
  • Not supported by empirical evidence
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13
Q

What does a volatility model describe ?

A

Evolution of σ(t)^2

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14
Q

What are the 2 types of volatility models ?

A
  • Volatility = exact function → (G)ARCH models

* Volatility = stochastic function → stochastic volatility models

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15
Q

What is the basic idea of an ARCH model ?

A

Unexpected return is serially uncorrelated but dependent where the dependency is a quadratic funtion of lagged values

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16
Q

How is forecasting obtained on an ARCH model ?

A

Recursively

17
Q

What is the characterisic of the excess kurtosis in ARCH models ?

A

Always positive

18
Q

What are the ML estimation properties ?

A
  • Consistency
  • Asymptotic normality
  • Asymptotic efficiency
  • Invariance
19
Q

What is the drawback of the Hessian form of Î(θ) ?

A

It relies on second-order derivatives of log-likelihood → measure very erratic.

20
Q

What is the alternative of the hessian form ?

A

Use an alternative estimator of I(θ) based on first order derivatives called BHHH estimator or outer product of gradients estimator.

21
Q

What are the various steps for estimation ?

A
  1. Estimate mean equation
  2. Select initial values for θ
  3. Compute conditional volatility
  4. Compute log-likelihood
  5. Change values of parameters
  6. Iterate steps 3-5 until convergence
22
Q

What test is used for ARCH effects ?

A

The Lagrange Multiplier

23
Q

What is the null of the LM test on ARCH ?

A

Ho : ϵt|It-1 ̴ N(0,σ^2) based on : α1 = … = αp = 0

24
Q

What is the alternative of the LM test on ARCH ?

A

Ha : ϵt|It-1 ̴ ARCH(p) based on : αi ≥ 0 with at least on strict inequality.

25
Q

What is the LM test statistic ?

A

TR^2 where T is the sample size & R^2 is computed from ϵ_t^2=α_0+α_1 ϵ_(t-1)^2+⋯+ α_p ϵ_(t-p)^2+v_t
It is distributed as a X^2(p)

26
Q

What is an alternative to the LM test ?

A

Ljung-Box for ϵ_t^2 with p lags → X^2(p)

27
Q

What are the limits to the ARCH Models ?

A
  • Need many lags to capture dynamics of volatility
  • Complicated constraints on parameters for series to be well behaved

• Positive & Negative shocks assumed to have same effect on volatility
→ In general negative shocks stronger effect on volatility

• Likely to overpredict volatility because respond slowly to large isolated shocks to return series