# Zambia rainy-season extremes: flood and dry-spell risk, 1981–2026
Have Zambia's rainy-season dry spells, wet spells and extreme-rainfall totals shifted over
the past 45 seasons — and if so, where?
Short answer: **almost nothing is statistically significant on its own, but the direction of
change is remarkably consistent, and it points to a redistribution rather than a simple
wetting or drying.** Rain is falling on *more* days and adding up to *more* total, while the
heaviest single-day downpours *weaken* and the longest dry spell *within* the season gets
*longer*. For rain-fed agriculture that combination matters more than the seasonal total does.
> **Companion study — zambia-temperature-extremes →**
> The same test, run on ERA5 temperature over the same country and the same 45 years,
> gives the opposite answer: the hottest day of the year is rising in **all ten provinces**,
> and in **this same ONDJFM window 969 grid cells survive false-discovery-rate control**
> against **zero** for any rainfall index. That contrast is what makes the rainfall null
> result below credible rather than merely inconclusive.
*Trend per decade in each index, 1981/82–2025/26. Blue is wetter, red is drier, throughout —
CDD uses a reversed scale because a **rising** dry spell means a **drier** season. Stippled
cells are significant at p < 0.05 before multiple-testing control (see Finding 2).*
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## The question, and why it is framed this way
Zambia's rains fall in a single wet season, **ONDJFM** — 1 October to 31 March. Almost all
national crop production depends on it. Two things can go wrong inside a season that a
rainfall *total* completely hides:
- a **dry spell** long enough to kill a crop mid-season, even in a wet year
- a **cloudburst** heavy enough to flood, even in a dry year
So the analysis is built on spell-length and percentile-exceedance indices rather than
totals, and every index is computed over the ONDJFM window only. A season is labelled by its
**start** yea …