Summary
A short, influential paper giving a fully Bayesian treatment of a Poisson process with a single change-point at an unknown time: the event rate is λ1 before the change and λ2 after, and the change occurs at unknown t. Raftery and Akman derive the joint posterior of (λ1,λ2,t) under Gamma priors, and — the paper's methodological hook — construct a Bayes factor to test whether a change-point exists at all (constant-rate model M0 vs. change-point model M1), including a device for making the test well-defined under vague/improper priors. The classic coal-mining disasters series is the illustration, locating the change around 1890.
Key Claims
- Model. On [0,T] with n events at times t1,…,tn, the rate is λ(s)=λ1 for s≤t and λ2 for s>t; conjugate Gamma priors on the rates give a closed-form posterior for (λ1,λ2) given t, and the marginal posterior of the change-point t (a discrete-plus-continuous object over the inter-event intervals).
- Magnitude of change. The posterior of β=λ2/λ1 (the ratio of rates) is obtained; it summarizes how big the change was, separately from when.
- Bayes factor for existence of a change. Testing is framed as model comparison: M0 (constant rate) vs. M1 (one change-point), with the Bayes factor B01=p(t∣M0)/p(t∣M1) built from the two integrated likelihoods.
- Improper-prior fix (imaginary observation). With vague priors the Bayes factor contains an arbitrary ratio of prior constants c0/c1 and is not well-defined. Raftery-Akman adopt the Spiegelhalter-Smith (1982) boundary-condition device: fix the constant so that the smallest data set maximally favouring M0 (a single event halfway through [0,T]) yields a Bayes factor just above one. Under Jeffreys-type priors (bk=−21) this pins down c01(T) and gives an operational, scale-invariant test.
- Coal-mining example. On Jarrett's (1979) corrected British coal-mining disaster series (1851–1962), the change-point posterior has mode 10 March 1890, median 27 August 1890, 95% region [15 May 1887, 3 August 1895]; the rate-ratio β has posterior mean 3.41 (95% HPD [2.48,4.46]) — a roughly 3.4-fold drop in disaster rate after 1890.
Concepts Introduced or Extended
Entities Mentioned
Quotes
"A Bayesian approach to estimation and hypothesis testing for a Poisson process with a change-point is developed, and an example given."
"The boundary condition is that a data set which involves the smallest possible sample size permitting a comparison of M0 and M1 and provides maximum possible support for M0 should yield a Bayes factor which is only very slightly greater than one."
My Take
This is a small paper that punches above its length: it fixes the coal-mining change-point as the canonical worked example that Carlin-Gelfand-Smith (1992), Barry-Hartigan (1993), and Green's (1995) reversible-jump treatment all return to, and it gets a clean answer (a ~3.4× rate drop near 1890) from conjugate Gamma-Poisson algebra alone — no MCMC needed for a single change-point. Its genuinely reusable idea is the improper-prior Bayes factor problem and the Spiegelhalter-Smith imaginary-observation calibration: because a diffuse prior leaves an undetermined constant in the marginal likelihood, "does a change exist?" is ill-posed until you anchor that constant, and their boundary-condition trick is an early, concrete instance of the intrinsic/fractional-Bayes-factor ideas that later formalized model comparison under vague priors. For the wiki it is the single-change-point Bayesian precedent underneath the change-point concept, the fixed point the trans-dimensional methods generalize.