Botswana vs Iraq: Open shrubland — Burning crop residues
Botswana
13.21 million t
in 2024
Iraq
1.33 million t
in 2024
Botswana rank
5th
Iraq rank
7th
Open shrubland — Burning crop residues over time
- Botswana
- Iraq
How they compare
Botswana currently reports 13.21 million t against 1.33 million t in Iraq, a difference of 11.88 million t.
That makes Botswana's figure about 9.9 times Iraq's.
Across all 35 years both countries report, Botswana has been ahead every year.
Botswana ranks 5th and Iraq ranks 7th of 218 countries.
Botswana has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Botswana | Iraq | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 18.68 million t | 392,827 t | 18.29 million t | Botswana |
| 2000s | 21.95 million t | 56,029 t | 21.89 million t | Botswana |
| 2010s | 30.73 million t | 277,425 t | 30.45 million t | Botswana |
| 2020s | 49.34 million t | 535,457 t | 48.80 million t | Botswana |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher open shrubland — burning crop residues, Botswana or Iraq?
- Botswana, at 13.21 million t against 1.33 million t in Iraq as of 2024.
- What is the difference in open shrubland — burning crop residues between Botswana and Iraq?
- 11.88 million t, with Botswana ahead.
- How many years of comparable data are there for Botswana and Iraq?
- 35 years are reported by both, from 1990 to 2024.
- How do Botswana and Iraq rank globally for open shrubland — burning crop residues?
- Botswana ranks 5th and Iraq ranks 7th of 218 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Open 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.