Bhutan vs Mongolia: Savanna and woody savanna — Burning crop residues
Bhutan
9,322 t
in 2024
Mongolia
7,195 t
in 2024
Bhutan rank
86th
Mongolia rank
88th
Savanna and woody savanna — Burning crop residues over time
- Bhutan
- Mongolia
How they compare
Bhutan currently reports 9,322 t against 7,195 t in Mongolia, a difference of 2,127 t.
That makes Bhutan's figure about 1.3 times Mongolia's.
The two have swapped places 9 times across 35 shared years of data; in 1990 it was Mongolia ahead.
Bhutan ranks 86th and Mongolia ranks 88th of 221 countries.
Across the 4 decades both report, Bhutan averaged higher in 1 and Mongolia in 3.
Head to head by decade
| Decade | Bhutan | Mongolia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 6,816 t | 121,402 t | 114,585 t | Mongolia |
| 2000s | 5,247 t | 186,386 t | 181,139 t | Mongolia |
| 2010s | 12,110 t | 104,350 t | 92,240 t | Mongolia |
| 2020s | 6,184 t | 2,850 t | 3,334 t | Bhutan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna and woody savanna — burning crop residues, Bhutan or Mongolia?
- Bhutan, at 9,322 t against 7,195 t in Mongolia as of 2024.
- What is the difference in savanna and woody savanna — burning crop residues between Bhutan and Mongolia?
- 2,127 t, with Bhutan ahead.
- How many years of comparable data are there for Bhutan and Mongolia?
- 35 years are reported by both, from 1990 to 2024.
- How do Bhutan and Mongolia rank globally for savanna and woody savanna — burning crop residues?
- Bhutan ranks 86th and Mongolia ranks 88th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Savanna and 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.