Forward probability
The likelihood asks how often warm sea-surface temperatures occur when a cyclone does or does not form.
From prior belief to posterior probability
Bayes' theorem combines what was plausible before an observation with how compatible that observation is under each possible explanation.
The essential idea: evidence updates probability through likelihood, but the base rate still matters.
The likelihood asks how often warm sea-surface temperatures occur when a cyclone does or does not form.
The posterior asks how likely cyclone formation is after warm SST has been observed.
Use the tropical-cyclone example from the video. Change the base rate and the two likelihoods, then watch the posterior update.
| Cyclone | No cyclone | |
|---|---|---|
| Warm SST | 45 | 285 |
| Cooler SST | 5 | 665 |
A strong indicator can still imply a modest posterior probability when the event itself is rare or false positives are common.