Savanna — Burning crop residues in Mongolia
Mongolia: Savanna — Burning crop residues was 3,356 t in 2024. ◆ Volatile
Savanna — Burning crop residues in Mongolia, 1990–2024
Source: Food and Agriculture Organization of the United Nations. Measured in t.
Analysis
In 2024, savanna — burning crop residues in Mongolia stood at 3,356 t.
Compared with earlier readings it is up 2.7% on the previous year and up 26.7% over ten years.
Over the whole period, savanna — burning crop residues in Mongolia peaked at 312,669 t in 2012 and was at its lowest, 0 t, in 2021.
That places Mongolia 91st out of 221 countries with data for 2024, putting it in the middle of the range.
The series is highly variable year to year, so single readings are best treated with caution.
Savanna — Burning crop residues in Mongolia, year by year
| Year | t | Change |
|---|---|---|
| 1990 | 49,449 t | — |
| 1991 | 49,449 t | +0.0% |
| 1992 | 49,449 t | +0.0% |
| 1993 | 49,449 t | +0.0% |
| 1994 | 49,449 t | +0.0% |
| 1995 | 49,449 t | +0.0% |
| 1996 | 6,492 t | -86.9% |
| 1997 | 66,631 t | +926.3% |
| 1998 | 12,571 t | -81.1% |
| 1999 | 7,707 t | -38.7% |
| 2000 | 12,624 t | +63.8% |
| 2001 | 2,649 t | -79.0% |
| 2002 | 101,981 t | +3749.8% |
| 2003 | 61,368 t | -39.8% |
| 2004 | 5,739 t | -90.6% |
| 2005 | 21,545 t | +275.4% |
| 2006 | 37,613 t | +74.6% |
| 2007 | 110,107 t | +192.7% |
| 2008 | 279,440 t | +153.8% |
| 2009 | 152,592 t | -45.4% |
| 2010 | 2,737 t | -98.2% |
| 2011 | 19,605 t | +616.3% |
| 2012 | 312,669 t | +1494.8% |
| 2013 | 4,238 t | -98.6% |
| 2014 | 2,650 t | -37.5% |
| 2015 | 67,110 t | +2432.8% |
| 2016 | 1,589 t | -97.6% |
| 2017 | 56,062 t | +3427.4% |
| 2018 | 2,296 t | -95.9% |
| 2019 | 76,724 t | +3241.5% |
| 2020 | 2,649 t | -96.5% |
| 2021 | 0 t | -100.0% |
| 2022 | 0 t | — |
| 2023 | 3,267 t | — |
| 2024 | 3,356 t | +2.7% |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 39,009 t | 6,492 t | 66,631 t | 10 |
| 2000s | 78,566 t | 2,649 t | 279,440 t | 10 |
| 2010s | 54,568 t | 1,589 t | 312,669 t | 10 |
| 2020s | 1,854 t | 0 t | 3,356 t | 5 |
Countries ranked near Mongolia
More climate change data for Mongolia
- Emissions from livestock — Emissions (CO2eq) 17,853 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 4,940 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 12,913 kt (2050)
- Emissions from livestock — Emissions 18.64 kt (2050)
- Emissions from livestock — Emissions 461.19 kt (2050)
- Emissions from crops — Emissions (CO2eq) 67.54 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 64.77 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 2.77 kt (2050)
- Emissions from crops — Emissions 0.2444 kt (2050)
- Emissions from crops — Emissions 0.0991 kt (2050)
Frequently asked questions
- What is savanna — burning crop residues in Mongolia?
- Savanna — burning crop residues in Mongolia was 3,356 t in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest savanna — burning crop residues recorded in Mongolia?
- The highest recorded value was 312,669 t in 2012.
- What is the lowest savanna — burning crop residues recorded in Mongolia?
- The lowest recorded value was 0 t in 2021.
- How does Mongolia rank for savanna — burning crop residues?
- Mongolia ranks 91st out of 221 countries with data for 2024.
- Is savanna — burning crop residues rising or falling in Mongolia?
- Over the last ten years it is up 26.7%. The long-run trend across the full record is volatile.
- Where does this Mongolia data come from?
- The figures come from Food and Agriculture Organization of the United Nations, published as part of Savanna — Burning crop residues (Biomass burned, dry matter). Statizoid updates them automatically from the source API.
Download this data
CSV · JSON — 35 observations, free to reuse under CC BY-NC-SA 3.0 IGO (FAO).
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.