 
 
 
 
 
   
We can easily extend Eqs. (73),
(77), and (79)
to a joint inference of several variables, which, as we
have seen, are nothing but parameters 
 of suitable models.  Using the alternative ways described in
Sects. 6.1 and 6.2, we have
of suitable models.  Using the alternative ways described in
Sects. 6.1 and 6.2, we have
Take a simple case of a common offset error
of an instrument used to measure various quantities  , 
resulting in the measurements
, 
resulting in the measurements  . We model each measurement as
. We model each measurement as  plus an error that is Gaussian distributed with a mean of zero and
a standard deviation
plus an error that is Gaussian distributed with a mean of zero and
a standard deviation  . The
calculation of the posterior distribution can be performed analytically,
with the following results (see D'Agostini 1999c for details):
. The
calculation of the posterior distribution can be performed analytically,
with the following results (see D'Agostini 1999c for details):
 is described by a Gaussian centered
at
 is described by a Gaussian centered
at  , with standard deviation
, with standard deviation 
 ,
consistent with Eq. (76).
,
consistent with Eq. (76).
 does not factorize
into the product of
 does not factorize
into the product of  ,
,  , etc., because correlations are
automatically introduced by the formalism, consistent with the
intuitive thinking of what a common systematic should do.
Therefore, the joint distribution will be a multi-variate Gaussian that
takes into account correlation terms.
, etc., because correlations are
automatically introduced by the formalism, consistent with the
intuitive thinking of what a common systematic should do.
Therefore, the joint distribution will be a multi-variate Gaussian that
takes into account correlation terms.
 is given by
is given by
|  |  |  | (84) | 
 has the behavior expected from a
 common offset error; it is  non-negative; it varies from
 practically zero, indicating negligible correlation, when 
(
 has the behavior expected from a
 common offset error; it is  non-negative; it varies from
 practically zero, indicating negligible correlation, when 
(
 ), to unity (
), to unity (
 ), 
when the offset error dominates.
), 
when the offset error dominates.
 
 
 
 
