Hans Bohlmann: I. The Classical Ratemaking Problem
Hans Bohlmann: I. The Classical Ratemaking Problem
Hans Bohlmann: I. The Classical Ratemaking Problem
E X P E R I E N C E RATING AND C R E D I B I L I T Y
HANS BOHLMANN
Ziirich
2. P r a g m a t i c Solution
Insurance people are practically minded, and so they have in
m a n y circumstances come out with pragmatic solutions, even if
the theoreticians were not able to provide them with full theore-
tical justification for doing so. Within the classical setup such
circumstances were happening if
200 EXPERIENCE RATING AND CREDIBILITY
- no claim bonus
-
But now let's turn to the second term in the heading of the
subject discussed: credibility.
It is quite remarkable that our American colleagues have been
well advised in solving most of their Experience Rating problems
in applying the by now famous credibility formula:
Pn = (i - - ~¢) pn-l+o~.rn-1
p~ : rate for period k
r, = loss ratio for period k
~t is called credibility and assumed to be a function of the
volume V, mostly
V I if V >~ Vo
= if V < Vo
V0 is called the volume offidl credibility.
Hetereogeneity in mass, in time, rate changes for big groups and
small groups as well, even some refund formulas are treated by
the credibility method on the United States m a r k e t - - a n d this is
the remarkable f a c t - - t h e credibility formula has been found to do
an excellent job. Under such circumstances it does not come as
a surprise that m a n y actuaries have tried to prove the credi-
bility formula starting from more general principles. The first to
do so was Arthur Bailey, one of the most outstanding A m e r i c a n
actuaries in the mid-century to whose work Bruno de Finetti has
drawn our attention at the Trieste colloquium. Since then I am sure
that many of us have made our own personal attempts. Edouard
Franckx in his paper "La ratification et son adaptation exp6riment-
ale dans le cadre d'une classe de tarif" arrives at the credibility
formula by starting from the principle of least squares. It seems to
me that in doing so he is the first author to prove the credibility
relation independent of the distribution function which governs the
individual risks (but still dependent on the prior distribution of the
risk parameter or parameters). This would justify our American
colleagues' using credibility procedures beyond the assessment
of claims frequencies--a point that since Arthur Bailey has worried
m a n y of our very best colleagues across the Atlantic.
I regret that there has been only one paper sent in which specifi-
204 EXPERIENCE RATING AND CREDIBILITY
where S(B) denotes the "a priori distribution" of the risk parameter
(structural function of portfolio), is smallest for the choice
f = E[tx(O~)/X1. . . . Xn].
I feel that the least expected square deviation is no sufficient
justification for the choice of the a posteriori mean as estimator
function. Permit me therefore to set forth another justification
which Paul Thyrion has indicated to me in a recent letter.
The basic idea can be described b y the postulate of equilibrium
in all those subclasses of a portfolio which are characterized by
experience only. In other words it is postulated that each class of
risks with equal observed risk performance should pay its own way.
Let us try to put this into mathematical language. Let
(9 = set of all possible parameters
X = set of all possible observed risk performances (Xi, X2,... Xn)
X' = subset of X, c(X') = cylinder in (9 × X with base X' c X
P = probability on (9 × X
F i n d : a, b such t h a t
X1 + X2 . . . . X n
a + b X where X7 =
n
a p p r o x i m a t e s E [ ~ ( 8 ) / x , , . . . x ~ best
i.e. E {E[~(8)/x,, x,, . . . x,~ - - (a + bX)} 2 = m i n i m u m
which is m i n i m u m if i) a = (I - - b)E[vt0) ]
a n d ii) b 2 E ( X - - ~t(8)) 2 + (I - - b) z Var Err(S)] mini-
mum
var[~O)]
which leads to b =
Var[t~(b)] + E ( X - - ~ ( ~ ) ) ~
A s s u m i n g n o w independence a n d identical d i s t r i b u t i o n of the
X , we find
I I
E(X-~O))~= -
n
E(X, -- ~(~))~ = -n E [ ~ ( 0 ) ]
where
n
b----
n+k
k--
Var[vt(8)]
Remarks: