Chad vs Western Europe: Savanna — Burning crop residues
Chad
1.57 million t
in 2024
Western Europe
529.34 t
in 2024
Chad rank
31st
Western Europe rank
30th
Savanna — Burning crop residues over time
- Chad
- Western Europe
How they compare
Chad currently reports 1.57 million t against 529.34 t in Western Europe, a difference of 1.57 million t.
That makes Chad's figure about 2,974.6 times Western Europe's.
Across all 35 years both countries report, Chad has been ahead every year.
Chad ranks 31st and Western Europe ranks 30th of 221 countries.
Chad has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Chad | Western Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 21.25 million t | 8,204 t | 21.24 million t | Chad |
| 2000s | 9.66 million t | 12,058 t | 9.65 million t | Chad |
| 2010s | 3.75 million t | 20,907 t | 3.73 million t | Chad |
| 2020s | 2.16 million t | 9,685 t | 2.15 million t | Chad |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, Chad or Western Europe?
- Chad, at 1.57 million t against 529.34 t in Western Europe as of 2024.
- What is the difference in savanna — burning crop residues between Chad and Western Europe?
- 1.57 million t, with Chad ahead.
- How many years of comparable data are there for Chad and Western Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do Chad and Western Europe rank globally for savanna — burning crop residues?
- Chad ranks 31st and Western Europe ranks 30th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as 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.