El Salvador vs Mongolia: Savanna — Burning crop residues
El Salvador
4,790 t
in 2024
Mongolia
3,356 t
in 2024
El Salvador rank
89th
Mongolia rank
91st
Savanna — Burning crop residues over time
- El Salvador
- Mongolia
How they compare
El Salvador currently reports 4,790 t against 3,356 t in Mongolia, a difference of 1,434 t.
That makes El Salvador's figure about 1.4 times Mongolia's.
The two have swapped places 11 times across 35 shared years of data; in 1990 it was Mongolia ahead.
El Salvador ranks 89th and Mongolia ranks 91st of 221 countries.
Across the 4 decades both report, El Salvador averaged higher in 1 and Mongolia in 3.
Head to head by decade
| Decade | El Salvador | Mongolia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 8,630 t | 39,009 t | 30,379 t | Mongolia |
| 2000s | 9,546 t | 78,566 t | 69,019 t | Mongolia |
| 2010s | 22,445 t | 54,568 t | 32,123 t | Mongolia |
| 2020s | 8,401 t | 1,854 t | 6,546 t | El Salvador |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, El Salvador or Mongolia?
- El Salvador, at 4,790 t against 3,356 t in Mongolia as of 2024.
- What is the difference in savanna — burning crop residues between El Salvador and Mongolia?
- 1,434 t, with El Salvador ahead.
- How many years of comparable data are there for El Salvador and Mongolia?
- 35 years are reported by both, from 1990 to 2024.
- How do El Salvador and Mongolia rank globally for savanna — burning crop residues?
- El Salvador ranks 89th and Mongolia ranks 91st 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.