Botswana vs Mexico: Closed shrubland — Burning crop residues
Botswana
423,395 t
in 2024
Mexico
124,851 t
in 2024
Botswana rank
7th
Mexico rank
10th
Closed shrubland — Burning crop residues over time
- Botswana
- Mexico
How they compare
Botswana currently reports 423,395 t against 124,851 t in Mexico, a difference of 298,544 t.
That makes Botswana's figure about 3.4 times Mexico's.
The two have swapped places 12 times across 35 shared years of data; in 1990 it was Botswana ahead.
Botswana ranks 7th and Mexico ranks 10th of 219 countries.
Across the 4 decades both report, Botswana averaged higher in 1 and Mexico in 3.
Head to head by decade
| Decade | Botswana | Mexico | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 676,294 t | 955,350 t | 279,056 t | Mexico |
| 2000s | 453,580 t | 535,609 t | 82,029 t | Mexico |
| 2010s | 1.48 million t | 321,295 t | 1.16 million t | Botswana |
| 2020s | 320,789 t | 366,532 t | 45,744 t | Mexico |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Botswana or Mexico?
- Botswana, at 423,395 t against 124,851 t in Mexico as of 2024.
- What is the difference in closed shrubland — burning crop residues between Botswana and Mexico?
- 298,544 t, with Botswana ahead.
- How many years of comparable data are there for Botswana and Mexico?
- 35 years are reported by both, from 1990 to 2024.
- How do Botswana and Mexico rank globally for closed shrubland — burning crop residues?
- Botswana ranks 7th and Mexico ranks 10th 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.