Angola vs World: Closed shrubland — Burning crop residues
Angola
7.12 million t
in 2024
World
18.70 million t
in 2024
Angola rank
4th
World rank
1st
Closed shrubland — Burning crop residues over time
- Angola
- World
How they compare
World currently reports 18.70 million t against 7.12 million t in Angola, a difference of 11.58 million t.
That makes World's figure about 2.6 times Angola's.
Across all 35 years both countries report, World has been ahead every year.
Angola ranks 4th and World ranks 1st of 219 countries.
World has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Angola | World | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 4.99 million t | 65.91 million t | 60.91 million t | World |
| 2000s | 10.78 million t | 72.13 million t | 61.35 million t | World |
| 2010s | 6.21 million t | 50.65 million t | 44.44 million t | World |
| 2020s | 5.43 million t | 31.72 million t | 26.29 million t | World |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Angola or World?
- World, at 18.70 million t against 7.12 million t in Angola as of 2024.
- What is the difference in closed shrubland — burning crop residues between Angola and World?
- 11.58 million t, with World ahead.
- How many years of comparable data are there for Angola and World?
- 35 years are reported by both, from 1990 to 2024.
- How do Angola and World rank globally for closed shrubland — burning crop residues?
- Angola ranks 4th and World ranks 1st 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.