Chad vs Oceania: Grassland — Burning crop residues
Chad
23.34 million t
in 2024
Oceania
101.34 million t
in 2024
Chad rank
10th
Oceania rank
10th
Grassland — Burning crop residues over time
- Chad
- Oceania
How they compare
Oceania currently reports 101.34 million t against 23.34 million t in Chad, a difference of 78.01 million t.
That makes Oceania's figure about 4.3 times Chad's.
Across all 35 years both countries report, Oceania has been ahead every year.
Chad ranks 10th and Oceania ranks 10th of 220 countries.
Oceania has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Chad | Oceania | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 21.37 million t | 72.63 million t | 51.26 million t | Oceania |
| 2000s | 35.46 million t | 124.80 million t | 89.34 million t | Oceania |
| 2010s | 31.72 million t | 102.28 million t | 70.55 million t | Oceania |
| 2020s | 27.23 million t | 83.41 million t | 56.18 million t | Oceania |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland — burning crop residues, Chad or Oceania?
- Oceania, at 101.34 million t against 23.34 million t in Chad as of 2024.
- What is the difference in grassland — burning crop residues between Chad and Oceania?
- 78.01 million t, with Oceania ahead.
- How many years of comparable data are there for Chad and Oceania?
- 35 years are reported by both, from 1990 to 2024.
- How do Chad and Oceania rank globally for grassland — burning crop residues?
- Chad ranks 10th and Oceania ranks 10th of 220 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland — 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.