Belarus vs Mongolia: Woody savanna — Burning crop residues
Belarus
3,130 t
in 2024
Mongolia
3,839 t
in 2024
Belarus rank
72nd
Mongolia rank
69th
Woody savanna — Burning crop residues over time
- Belarus
- Mongolia
How they compare
Mongolia currently reports 3,839 t against 3,130 t in Belarus, a difference of 709 t.
That makes Mongolia's figure about 1.2 times Belarus's.
The two have swapped places 6 times across 33 shared years of data; in 1992 it was Mongolia ahead.
Belarus ranks 72nd and Mongolia ranks 69th of 220 countries.
Across the 4 decades both report, Belarus averaged higher in 1 and Mongolia in 3.
Head to head by decade
| Decade | Belarus | Mongolia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 15,645 t | 85,812 t | 70,167 t | Mongolia |
| 2000s | 48,614 t | 107,820 t | 59,206 t | Mongolia |
| 2010s | 29,971 t | 49,782 t | 19,811 t | Mongolia |
| 2020s | 4,907 t | 995.24 t | 3,912 t | Belarus |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher woody savanna — burning crop residues, Belarus or Mongolia?
- Mongolia, at 3,839 t against 3,130 t in Belarus as of 2024.
- What is the difference in woody savanna — burning crop residues between Belarus and Mongolia?
- 709 t, with Mongolia ahead.
- How many years of comparable data are there for Belarus and Mongolia?
- 33 years are reported by both, from 1992 to 2024.
- How do Belarus and Mongolia rank globally for woody savanna — burning crop residues?
- Belarus ranks 72nd and Mongolia ranks 69th of 220 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Woody 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.