Chile vs Eastern Asia: Closed shrubland — Burning crop residues
Chile
8,593 t
in 2024
Eastern Asia
1,722 t
in 2024
Chile rank
18th
Eastern Asia rank
18th
Closed shrubland — Burning crop residues over time
- Chile
- Eastern Asia
How they compare
Chile currently reports 8,593 t against 1,722 t in Eastern Asia, a difference of 6,871 t.
That makes Chile's figure about 5.0 times Eastern Asia's.
The two have swapped places 5 times across 35 shared years of data; in 1990 it was Eastern Asia ahead.
Chile ranks 18th and Eastern Asia ranks 18th of 219 countries.
Across the 4 decades both report, Chile averaged higher in 2 and Eastern Asia in 2.
Head to head by decade
| Decade | Chile | Eastern Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 98,037 t | 214,911 t | 116,874 t | Eastern Asia |
| 2000s | 26,583 t | 56,044 t | 29,461 t | Eastern Asia |
| 2010s | 53,974 t | 11,969 t | 42,005 t | Chile |
| 2020s | 48,811 t | 1,377 t | 47,434 t | Chile |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Chile or Eastern Asia?
- Chile, at 8,593 t against 1,722 t in Eastern Asia as of 2024.
- What is the difference in closed shrubland — burning crop residues between Chile and Eastern Asia?
- 6,871 t, with Chile ahead.
- How many years of comparable data are there for Chile and Eastern Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Chile and Eastern Asia rank globally for closed shrubland — burning crop residues?
- Chile ranks 18th and Eastern Asia ranks 18th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed 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.