Chad vs Zimbabwe: Savanna — Burning crop residues
Chad
1.57 million t
in 2024
Zimbabwe
1.23 million t
in 2024
Chad rank
31st
Zimbabwe rank
34th
Savanna — Burning crop residues over time
- Chad
- Zimbabwe
How they compare
Chad currently reports 1.57 million t against 1.23 million t in Zimbabwe, a difference of 340,640 t.
That makes Chad's figure about 1.3 times Zimbabwe's.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was Chad ahead.
Chad ranks 31st and Zimbabwe ranks 34th of 221 countries.
Chad has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Chad | Zimbabwe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 21.25 million t | 11.51 million t | 9.75 million t | Chad |
| 2000s | 9.66 million t | 3.82 million t | 5.84 million t | Chad |
| 2010s | 3.75 million t | 3.16 million t | 590,214 t | Chad |
| 2020s | 2.16 million t | 1.26 million t | 900,191 t | Chad |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, Chad or Zimbabwe?
- Chad, at 1.57 million t against 1.23 million t in Zimbabwe as of 2024.
- What is the difference in savanna — burning crop residues between Chad and Zimbabwe?
- 340,640 t, with Chad ahead.
- How many years of comparable data are there for Chad and Zimbabwe?
- 35 years are reported by both, from 1990 to 2024.
- How do Chad and Zimbabwe rank globally for savanna — burning crop residues?
- Chad ranks 31st and Zimbabwe ranks 34th 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.