Glossary

Glossary

The scores, methods and terms used on the site. On every page, the first use of a term shows its explanation when you point at it (or reach it with the keyboard).

Benjamini–Hochberg
Benjamini–Hochberg correction for testing many methods or targets at once: controls the expected share of false findings among those confirmed (less strict than Holm). The method selection uses it since 17 October 2026.
BSS
Brier skill score of the probability of one category (e.g. below normal) against climatology. Positive is better than climatology.
CHIRPS
Climate Hazards Center InfraRed Precipitation with Stations: the gridded observed rainfall (0.05°, averaged to 0.25°) used for calibration and verification.
climatology
The reference forecast: the observed frequency of each tercile in the training years (about one-third each), or the past observed totals for amounts.
climatology blend
The final probabilities mix the model probabilities with climatology: p = (1 − λ)·p_model + λ·p_climatology, one weight λ per target fitted on past years.
coverage
Share of observations inside the forecast 10–90% range; 80% is calibrated, less means the range is too narrow.
cross-validated
Each year is forecast with parameters fitted without that year (leave-one-year-out), so the score is not inflated by fitting to the year itself.
CRPS
Continuous ranked probability score of a rainfall-amount forecast (ensemble or distribution) against the observed total, in mm. Lower is better.
CRPSS
Continuous ranked probability skill score for rainfall amounts: 1 − CRPS of the forecast / CRPS of climatology. Positive is better than climatology.
EMOS
Ensemble model output statistics: a regression that turns the raw ensemble into a full rainfall distribution (here a censored shifted gamma).
exploratory
Scores of years that were seen while the method was chosen (2017 onward); useful context, but weaker evidence than the cross-validated 1993–2016 scores.
Holm
Holm correction for testing many methods or targets at once: p-values are adjusted so that a confirmation is not a chance result of the number of tests.
leave-one-year-out
Each year is left out in turn; everything is fitted on the other years and the left-out year is scored.
Mean-Variance Scaling
MVS, the operational amount correction: each member is shifted and scaled so the model mean and spread match CHIRPS in every grid cell (spread ratio limited to 0.5–2).
MVS
Mean-Variance Scaling, the operational amount correction: each member is shifted and scaled so the model mean and spread match CHIRPS in every grid cell.
pinball loss
The score of one forecast quantile (e.g. the median) against the observation; lower is better.
rainfall domain
The area where the season matters climatologically (e.g. FMAM ≥ 100 mm and ≥ 20% of annual rainfall); used for summaries and maps, not for calibration.
reliability
Whether events forecast with probability p happen p of the time; a reliability diagram plots observed frequency against forecast probability.
RPS
Ranked probability score of tercile probabilities against the observed category (cumulative, so near misses cost less). Lower is better.
RPSS
Ranked probability skill score: 1 − RPS of the forecast / RPS of climatology. Positive is better than climatology; +0.05 means a 5% lower score.
SEAS5
ECMWF seasonal forecast system 5 (system 51): 25 members in the 1993–2016 hindcasts, 51 from 2017.
shadow forecast
A forecast made every cycle with an alternative method and scored against observations, but never published; it collects independent evidence.
spread–error
Ratio of the ensemble spread to the error of the ensemble mean; 1 means the spread matches the error, below 1 too narrow.
tercile
One of three equally likely categories of seasonal rainfall in the reference period: below normal, near normal, above normal.