Chile vs Colombia: Closed and open shrubland — Burning crop residues
Chile
12,584 t
in 2024
Colombia
8,560 t
in 2024
Chile rank
33rd
Colombia rank
35th
Closed and open shrubland — Burning crop residues over time
- Chile
- Colombia
How they compare
Chile currently reports 12,584 t against 8,560 t in Colombia, a difference of 4,024 t.
That makes Chile's figure about 1.5 times Colombia's.
The two have swapped places 9 times across 35 shared years of data; in 1990 it was Colombia ahead.
Chile ranks 33rd and Colombia ranks 35th of 219 countries.
Across the 4 decades both report, Chile averaged higher in 2 and Colombia in 2.
Head to head by decade
| Decade | Chile | Colombia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 122,407 t | 307,275 t | 184,869 t | Colombia |
| 2000s | 47,384 t | 112,648 t | 65,264 t | Colombia |
| 2010s | 80,100 t | 16,890 t | 63,211 t | Chile |
| 2020s | 59,920 t | 5,250 t | 54,670 t | Chile |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Chile or Colombia?
- Chile, at 12,584 t against 8,560 t in Colombia as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Chile and Colombia?
- 4,024 t, with Chile ahead.
- How many years of comparable data are there for Chile and Colombia?
- 35 years are reported by both, from 1990 to 2024.
- How do Chile and Colombia rank globally for closed and open shrubland — burning crop residues?
- Chile ranks 33rd and Colombia ranks 35th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed and open shrubland — Burning crop residues (Biomass burned, dry matter). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The FAOSTAT domain on Emissions from Fires consists of estimates of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from biomass burning in a range of vegetation types and from fires in organic soils.