Asia vs Zambia: Forest fires — Burning crop residues
Asia
198.97 million t
in 2024
Zambia
157.72 million t
in 2024
Asia rank
4th
Zambia rank
2nd
Forest fires — Burning crop residues over time
- Asia
- Zambia
How they compare
Asia currently reports 198.97 million t against 157.72 million t in Zambia, a difference of 41.25 million t.
That makes Asia's figure about 1.3 times Zambia's.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was Asia ahead.
Asia ranks 4th and Zambia ranks 2nd of 22 groups.
Asia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Asia | Zambia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 231.22 million t | 103.78 million t | 127.44 million t | Asia |
| 2000s | 254.18 million t | 134.45 million t | 119.73 million t | Asia |
| 2010s | 264.00 million t | 214.51 million t | 49.48 million t | Asia |
| 2020s | 221.38 million t | 153.05 million t | 68.32 million t | Asia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher forest fires — burning crop residues, Asia or Zambia?
- Asia, at 198.97 million t against 157.72 million t in Zambia as of 2024.
- What is the difference in forest fires — burning crop residues between Asia and Zambia?
- 41.25 million t, with Asia ahead.
- How many years of comparable data are there for Asia and Zambia?
- 35 years are reported by both, from 1990 to 2024.
- How do Asia and Zambia rank globally for forest fires — burning crop residues?
- Asia ranks 4th and Zambia ranks 2nd of 22 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Forest fires — 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.