A national wildfire consequence model. Given an ignition, a landscape and a day's weather, it returns a distribution of priced outcomes rather than a single footprint.
Forty seasons of CONAF's national record show a regime that changed. Not by having more fires. By having bigger ones.
Two seasons carry most of that 2.9×. 2016–17 (570,197 ha) and 2022–23 (429,103 ha) hold 61% of everything burned in the decade, and both sit far outside anything in the previous thirty years, whose worst season was 105,992 ha. Take those two out and the remaining eight average 78,432 hectares a year, still 1.4× the 1985–2014 mean, and the decade's median is still 1.8× the earlier median. The trend across all 40 seasons stays positive on both series: +44 fires per year (p < 0.001) and +2,946 hectares per year (p = 0.035). The regime did change. The 2.9× is that change plus two extraordinary years.
The national registry carries 109,985 georeferenced starts between July 2002 and June 2020. Inside the modelled surface sit 10.66 million building footprints and 16.16 million people. The ignition model's strongest predictors are temperature, population, distance to settlement and plantation fraction.
A gradient-boosted classifier on hexagon-days, trained on the national registry with deliberate burning removed. PR-AUC 0.884, ROC-AUC 0.962.
Final size is predicted as a continuous distribution of percentiles, not a point estimate that the physics cannot support. Any percentile between the 50th and the 95th can be asked for directly.
A stochastic susceptible-infected-recovered automaton on the landscape raster, with a fuel, slope and wind rate-of-spread as a susceptibility prior. Many runs give a burn-probability field.
The probability field is multiplied by cost surfaces and summed over the footprint. Four terms: human safety, structures, suppression keyed to fuel, and land restoration.
Most fire models stop at property damage. SWIM carries an explicit loss-of-life term inside the same footprint: population density under the burn-probability field, at a fatality rate fitted from reported deaths in Chilean wildfires. It is the same calculation that answers where it will hurt, not only what it will cost.
Each recorded fire is rerun from its own ignition on its own day's conditions. The predicted area is scored on whether the fire that actually happened falls inside it. For a risk product the failure that matters is real fire outside the prediction, so the measure is how much of the burn lands inside, reported next to how many times larger the predicted area is than the burned one.
| Fire | Burned | Percentile | Predicted area | Predicted ÷ burned | Burn inside |
|---|---|---|---|---|---|
Santa Apolonia |
7,708 ha | p90 | 24,578 ha | 3.19× | 100.0% |
Pichaco |
5,518 ha | p95 | 54,497 ha | 9.88× | 100.0% |
Alto Nilahue |
5,463 ha | p95 | 46,738 ha | 8.55× | 100.0% |
El Carrizo |
14,173 ha | p95 | 41,062 ha | 2.90× | 95.7% |
Tabunco / El Águila |
3,215 ha | p95 | 6,911 ha | 2.15× | 92.4% |
Four fires are a demonstration rather than a statistical validation. They were chosen because between them they cover the axes on which a spread model fails: scale (El Carrizo at 14,173 ha), extreme wind (Santa Apolonia, on the worst day in the record), width of the percentile distribution (Alto Nilahue, contained but loose) and benign terrain (Tabunco, the tight case). All four were run on the same code, the same size model and their own day's conditions, with no per-fire tuning.
The same engine, run everywhere at once. Continental Chile is covered by 4,384,252 hexagons of 250 metres a side, 16.24 hectares each, and every hexagon carries its own answer to one question: if a fire starts here, what should it be expected to cost in an average year?
Multiply the first three terms and add the fourth, for every hexagon on every day of the year, and you have the map. A hexagon scores high only if fires start there, and they grow, and there is something to lose. All three have to be true at once: fuel with no people is cheap, people with no fuel are safe.
An expected value should land on the long-run average year, and this one does: within 12% of CONAF's 40-season mean and within 8% of the typical season of the last decade. Nothing was fitted to these numbers, the national ignition rate is pinned by the King–Zeng prior correction and size comes from the percentile distribution. What an expectation deliberately does not do is chase 2016–17 or 2022–23. A mean that reproduced those seasons would be wrong about every other one; those years live in the tail of the distribution, not at its centre.
Most starts never become fires. The ignition model counts every registered start, median final size 0.3 hectares. The size model is trained on fires that reached 10 hectares, mean 200. An escape probability splits them, and the national check reproduces the observed mean size of a Chilean ignition, 14.3 hectares, rather than pricing every roadside grass start as a 200 hectare event.
| Layer | Coverage |
|---|---|
| Fire perimeters | 1985 to 2018 · 8,153 fires |
| Ignition registry | 2002 to 2020 · 109,985 starts |
| Occurrence statistics | 1985 to 2024 |
| Active-fire detections | 2001 to present |
| Event delineations | 2017, 2023, 2024, 2026 |
| Fuels | 2021 · 10 m |
| Land-use history | 1950 to 2020 |
| Fuel models | current |
| Terrain | current · 30 m |
| Climate grids | 1960 to 2021 |
| Daily weather | 2002 to present |
| Station observations | 120 + 433 stations |
| Buildings | 2026-07 · 10,655,379 |
| Population | 2024 |
| Wildland-urban interface | current |
| Roads and transmission | 14,038 road features |
| Valuation | 2000 to 2026 |
| Base geometry | current |