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q-Credibility OLIVIER LE COURTOIS EMLyon Business School First - - PowerPoint PPT Presentation

q-Credibility OLIVIER LE COURTOIS EMLyon Business School First Version Outline of the Talk Parametric approach Non-parametric approach Semi-parametric approach q-Credibility OLIVIER LE COURTOIS First Version n q-Credibility that extends


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SLIDE 1

q-Credibility

OLIVIER LE COURTOIS EMLyon Business School

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SLIDE 2

First Version

Outline of the Talk

Parametric approach Non-parametric approach Semi-parametric approach

q-Credibility OLIVIER LE COURTOIS

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SLIDE 3

First Version

Parametric Approach

We want to solve the following program: min

α0,q,{αi},{βi} E

    α0,q +

n

i=1

αiXi +

n

i=1

βiX2

i − E(Xn+1|θ)

 

2

  . that extends credibility theory to a quadratic setting.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 4

First Version

Classic Notation

For hypothetical means: µ(θ) = E(X|θ), µ = E(µ(θ)). For the process variance: v(θ) = Var(X|θ), v = E(v(θ)). For the variance of hypothetical means: a = Var(µ(θ)). Then, Cov(Xi, Xk) = a, ∀i ̸= k, and, Cov(Xi, Xi) = Var(Xi) = a + v.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 5

First Version

Additional Notation

By analogy, we define Cov(X2

i , Xk) = b,

∀i ̸= k, and Cov(X2

i , Xi) = b + g,

and also Cov(X2

i , X2 k) = c,

∀i ̸= k, and Cov(X2

i , X2 i ) = Var(X2 i ) = c + h.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 6

First Version

q-Credibility Premium

We have: Pq = α0,q + Zq¯ X + YqX2, where α0,q = µ(1 − Zq) − Yq(µ2 + a + v), and Zq = n [ a(nc + h) − b(nb + g) ] (na + v)(nc + h) − (nb + g)2 , and Yq = n(bv − ag) (na + v)(nc + h) − (nb + g)2 .

q-Credibility OLIVIER LE COURTOIS

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First Version

q-Credibility Premium

We also have: Pq = µ + Zq(¯ X − µ) + Yq(X2 − (µ2 + v + a)).

q-Credibility OLIVIER LE COURTOIS

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SLIDE 8

First Version

Remark

When b = g = 0, without any constraint on c or h, then Zq =

na na+v = n n+ v

a , Yq = 0 and α0,q = µ(1 − Zq),

so we recover the classic credibility case.

q-Credibility OLIVIER LE COURTOIS

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First Version

Mean Square Error

The Mean Square Error is computed as follows: MSEq = E     α∗

0,q + n

i=1

α∗

i Xi + n

i=1

β∗

i X2 i − E(Xn+1|θ)

 

2

  , yielding MSEq = nv(ac − b2) + a(hv − g2) n2(ac − b2) + n(ah + cv − 2bg) + hv − g2 . In the classic context, the formula reduces to MSE = va na + v. The relative gain in MSE is measured by the quantity: κ = MSE − MSEq MSE .

q-Credibility OLIVIER LE COURTOIS

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First Version

Conditional Poisson Case

Denote θ as λ and X as N and assume that N conditional on λ is Poisson distributed. µ = v = E(λ) and a = Var(λ) in classic credibility theory. Then, b = a + E(λ3) − E(λ2) E(λ), and g = E(λ) + 2E(λ2), and also c = 2b − a + Var(λ2), and h = E(λ) + 6E(λ2) + 4E(λ3).

q-Credibility OLIVIER LE COURTOIS

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First Version

Poisson-Gamma Case

q-credibility reduces to classic credibility, with Yq = 0, and Zq = Z, and also α0,q = α0 = µ(1 − Z).

q-Credibility OLIVIER LE COURTOIS

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First Version

Poisson-Single Pareto Case

Let λ be single Pareto-distributed with parameters (η > 4, χ). We know that µ = v =

ηχ η−1 and a = ηχ2 η−2 −

(

ηχ η−1

)2 . Then, g =

ηχ η−1 + 2 ηχ2 η−2,

b = ηχ3

η−3 − ηχ2 η−2 ηχ η−1,

and c = 2b − a + ηχ4 η − 4 − ( ηχ2 η − 2 )2 , and also h = ηχ η − 1 + 6 ηχ2 η − 2 + 4 ηχ3 η − 3.

q-Credibility OLIVIER LE COURTOIS

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First Version

Poisson-Single Pareto Case

Illustration

The parameters of the single Pareto distribution are η = 5 and χ = 4 and we assume that 5 claims have been observed in the past n = 2 years. Then, µ = 5 and ¯ X = 2.5. According to classic credibility theory, P = 4.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 14

First Version

Poisson-Single Pareto Case

Illustration

According to the q-credibility approach, Number of claims distrib. (3,2) (4,1) (5,0) X2 6.5 8.5 12.5 Pq 4.1314 4.1629 4.2259

q-Credibility OLIVIER LE COURTOIS

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SLIDE 15

First Version

Poisson-Single Pareto Case

Illustration

We have: MSE = 1, and MSEq = 0.9317, so that κ = 6.83%.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

The classic estimator of expected hypothetical means is ˆ µ = 1 rn

r

i=1 n

j=1

Xij, and that of expected process variance is ˆ v = 1 r(n − 1)

r

i=1 n

j=1

(Xij − ¯ Xi)2, where ¯ Xi = 1

n n

j=1

Xij is the empirical mean of past observations for insured i.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

The estimator of the variance of hypothetical means is ˆ a = 1 r − 1

r

i=1

(¯ Xi − ¯ X)2 − ˆ v n where ¯ X is the empirical mean of past observations for all insureds, which is equal to ˆ µ.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

The quadratic non-parametric estimators are given as follows. ˆ h = 1 r(n − 1)

r

i=1 n

j=1

( X2

ij − X2 i

)2 , where X2

i = 1 n n

j=1

X2

ij is the empirical mean of past squared

  • bservations for a given insured i.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

Then, ˆ c = 1 r − 1

r

i=1

( X2

i − X2

)2 − ˆ h n, where X2 = 1 rn

r

i=1 n

j=1

X2

ij

is the empirical mean of past squared observations for all insureds.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

Next, ˆ g = 1 r(n − 1)

r

i=1 n

j=1

(X2

ij − X2 i )(Xij − ¯

Xi), and ˆ b = 1 r − 1

r

i=1

(X2

i − X2)(¯

Xi − ¯ X) − ˆ g n.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 21

First Version

Non-Parametric Approach

Illustration

Assume r = n = 3 and we have the following data:    1 2 6 X = 1 10 13 1 1 1   , where each line is for a zone and each element is a number of yellow submarines observed at each time.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

Illustration

According to classic credibility theory, the number of yellow submarines observed in each zone is as follows. P1 ≈ 3.3932, and P2 ≈ 6.4274, and P3 ≈ 2.1795.

q-Credibility OLIVIER LE COURTOIS

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First Version

Non-Parametric Approach

Illustration

According to the q-credibility approach, we have: Pq,1 ≈ 2.3890, and Pq,2 ≈ 6.2613, and Pq,3 ≈ 2.2928. Relative changes ( Pq,i−Pi

Pi

)

i=1:3 are respectively −29.6%, −2.58%,

and 5.2%.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 24

First Version

Non-Parametric Approach

Illustration

We have: MSE = 3.1016, and MSEq = 2.7634, so that κ = 10.9%.

q-Credibility OLIVIER LE COURTOIS

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First Version

Semi-Parametric Approach

Situation where the distribution of X conditionally on θ is known. Here, we assume this conditional distribution to be of the Poisson type and X is denoted by N. Each ni describes the number of insureds for which i claims occurred.

q-Credibility OLIVIER LE COURTOIS

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First Version

Semi-Parametric Approach

In the classic setting, we have: ˜ µ = ˜ v =

+∞

i=0

i ni

+∞

i=0

ni = 1 M

+∞

i=0

ini, where M =

+∞

i=0

  • ni. Then,

˜ a =

+∞

i=0

(i − ˜ µ)2ni

+∞

i=0

ni − 1 − ˜ v = 1 M − 1

+∞

i=0

(i − ˜ µ)2ni − ˜ v.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 27

First Version

Semi-Parametric Approach

In the q-credibility setting, we have: ˜ g = 1 M

+∞

i=0

(2i2 − i)ni, and ˜ b = 1 M − 1

+∞

i=0

 i2 − 1 M

+∞

i=0

i2ni    i − 1 M

+∞

i=0

ini   ni − ˜ g,

q-Credibility OLIVIER LE COURTOIS

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SLIDE 28

First Version

Semi-Parametric Approach

Further, ˜ h = 1 M

+∞

i=0

(4i3 − 6i2 + 3i)ni, and ˜ c = 1 M − 1

+∞

i=0

 i2 − 1 M

+∞

i=0

i2ni  

2

ni − ˜ h.

q-Credibility OLIVIER LE COURTOIS

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SLIDE 29

First Version

Semi-Parametric Approach

Illustration

Assume we observed i ni 560 1 134 2 14 3 2

q-Credibility OLIVIER LE COURTOIS

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SLIDE 30

First Version

Semi-Parametric Approach

Illustration

We can estimate the expected future number of claims in the next period for an insured who incurred i claims. According to classic credibility theory: P = [0.2359 0.2388 0.2417 0.2446]. According to the q-credibility approach: Pq = [0.2376 0.2266 0.2722 0.3743].

q-Credibility OLIVIER LE COURTOIS

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First Version

Semi-Parametric Approach

Illustration

We have: MSE = 0.000681, and MSEq = 0.000585, so that κ = 14.1%.

q-Credibility OLIVIER LE COURTOIS