Asia vs OECD: Woody savanna — Burning crop residues
Asia
9.21 million t
in 2024
OECD
12.40 million t
in 2024
Asia rank
4th
OECD rank
3rd
Woody savanna — Burning crop residues over time
- Asia
- OECD
How they compare
OECD currently reports 12.40 million t against 9.21 million t in Asia, a difference of 3.19 million t.
That makes OECD's figure about 1.3 times Asia's.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was OECD ahead.
Asia ranks 4th and OECD ranks 3rd of 22 groups.
Across the 4 decades both report, Asia averaged higher in 2 and OECD in 2.
Head to head by decade
| Decade | Asia | OECD | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 16.84 million t | 26.26 million t | 9.41 million t | OECD |
| 2000s | 14.63 million t | 11.16 million t | 3.47 million t | Asia |
| 2010s | 12.29 million t | 9.29 million t | 3.00 million t | Asia |
| 2020s | 9.63 million t | 12.14 million t | 2.51 million t | OECD |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher woody savanna — burning crop residues, Asia or OECD?
- OECD, at 12.40 million t against 9.21 million t in Asia as of 2024.
- What is the difference in woody savanna — burning crop residues between Asia and OECD?
- 3.19 million t, with OECD ahead.
- How many years of comparable data are there for Asia and OECD?
- 35 years are reported by both, from 1990 to 2024.
- How do Asia and OECD rank globally for woody savanna — burning crop residues?
- Asia ranks 4th and OECD ranks 3rd of 22 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Woody savanna — 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.