Mexico vs Western Asia: Savanna — Burning crop residues
Mexico
3.15 million t
in 2024
Western Asia
51,085 t
in 2024
Mexico rank
25th
Western Asia rank
27th
Savanna — Burning crop residues over time
- Mexico
- Western Asia
How they compare
Mexico currently reports 3.15 million t against 51,085 t in Western Asia, a difference of 3.10 million t.
That makes Mexico's figure about 61.7 times Western Asia's.
Across all 35 years both countries report, Mexico has been ahead every year.
Mexico ranks 25th and Western Asia ranks 27th of 221 countries.
Mexico has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Mexico | Western Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.48 million t | 33,776 t | 1.45 million t | Mexico |
| 2000s | 2.54 million t | 14,936 t | 2.52 million t | Mexico |
| 2010s | 2.54 million t | 17,001 t | 2.52 million t | Mexico |
| 2020s | 2.33 million t | 74,522 t | 2.26 million t | Mexico |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, Mexico or Western Asia?
- Mexico, at 3.15 million t against 51,085 t in Western Asia as of 2024.
- What is the difference in savanna — burning crop residues between Mexico and Western Asia?
- 3.10 million t, with Mexico ahead.
- How many years of comparable data are there for Mexico and Western Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Mexico and Western Asia rank globally for savanna — burning crop residues?
- Mexico ranks 25th and Western Asia ranks 27th 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.