You finally filter out from the collection of trials all those with a particular measured C14 age, and look at the distributions of true calendar ages that generated it, compared against the measured
calendar age distribution each algorithm output.
Not exact matches
The withdrawal rules are different for inherited IRA accounts; generally you must begin taking
distributions from an inherited IRA in the
calendar year following the year of the IRA owner's death, both for traditional and Roth inherited IRAs, regardless of your
age.
Let us simplify the problem further and assume that the lab can estimate the RC
age on a sample (given an assumed initial mass fraction) with negligible error, and then consider how we generate the probability
distribution for
calendar date even when we have no laboratory measurement error to take into account.
In effect, for each
calendar date the constructors have built the conditional distribution of «RC age given Calendar Date
calendar date the constructors have built the conditional
distribution of «RC
age given
Calendar Date
Calendar Date».
The
distribution for the measurement of carbon - 14
age has (we're assuming) the same standard deviation for every
calendar year, so it's always that case that we get some particular carbon - 14 measurement that was «unlikely», since any particular value for the measurement error is unlikely.
Jeffreys» prior, which in effect converts length elements in 14C space to length elements in
calendar age space, may convert single length elements in 14C space to multiple length elements in
calendar age space when the same 14C
age corresponds to multiple
calendar ages, thus over-representing in the posterior
distribution the affected parts of the 14C error
distribution probability.
The problem is, what input
distribution do you use in the first step, to generate the true
calendar ages?
You submit a physical sample which has a particular true
calendar / C14
age combination — a random point on the calibration curve — with some input
distribution.
For each sampled true
calendar age, a 14C determination
age is sampled randomly from a Gaussian error
distribution.
But the problem as I see it is that whilst it is probably realistic to assume that some kind of local uniformity results from that process, that doesn't tell you what
calendar ages it spans nor what the shape of the
distribution in that region is.
If the measurement for carbon - 14
age has Gaussian error with standard deviation 100 (as seems about right for Nic's Fig. 2), and the measurement is rounded to one decimal place, and the calibration curve maps
calendar age 750 to carbon - 14
age 1000, then the probability of the observation being 1000.0 given that the
calendar age is 750 is 0.1 (for one decimal place) times the probability density at 1000 of a Gaussian
distribution with mean 1000 and standard deviation 100, which works out to 0.0004.
This can be demonstrated analytically directly from the definition of the Fisher Information for a single parameter space if a constant variance is assumed for the
distribution of RC
age given a
calendar date, and the «true»
calendar dates for testing are selected from a uniform
distribution.
Most of the information in that
distribution is from your knowledge of how the
ages of archaeological artefacts are distributed, and in particular that they are likely to be more uniform in
calendar age than C14
age.