Savanna — Burning crop residues in Belarus
Belarus: Savanna — Burning crop residues was 2,032 t in 2024. ◆ Volatile
Savanna — Burning crop residues in Belarus, 1992–2024
Source: Food and Agriculture Organization of the United Nations. Measured in t.
Analysis
The most recent figure for savanna — burning crop residues in Belarus is 2,032 t, measured in 2024.
Compared with earlier readings it is up 2,199.0% on the previous year and down 97.0% over ten years.
Over the whole period, savanna — burning crop residues in Belarus peaked at 131,693 t in 2002 and was at its lowest, 32.35 t, in 2000.
Belarus ranks 92nd of 221 countries on this measure, 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 Belarus, year by year
| Year | t | Change |
|---|---|---|
| 1992 | 25,666 t | — |
| 1993 | 25,666 t | +0.0% |
| 1994 | 25,666 t | +0.0% |
| 1995 | 25,666 t | +0.0% |
| 1996 | 183.78 t | -99.3% |
| 1997 | 196.92 t | +7.2% |
| 1998 | 207.35 t | +5.3% |
| 1999 | 1,750 t | +743.8% |
| 2000 | 32.35 t | -98.2% |
| 2001 | 14,051 t | +43338.1% |
| 2002 | 131,693 t | +837.3% |
| 2003 | 33,668 t | -74.4% |
| 2004 | 21,122 t | -37.3% |
| 2005 | 19,883 t | -5.9% |
| 2006 | 43,037 t | +116.4% |
| 2007 | 14,406 t | -66.5% |
| 2008 | 12,286 t | -14.7% |
| 2009 | 23,860 t | +94.2% |
| 2010 | 8,219 t | -65.6% |
| 2011 | 5,655 t | -31.2% |
| 2012 | 52,218 t | +823.4% |
| 2013 | 12,904 t | -75.3% |
| 2014 | 68,216 t | +428.7% |
| 2015 | 72,192 t | +5.8% |
| 2016 | 11,667 t | -83.8% |
| 2017 | 2,386 t | -79.5% |
| 2018 | 46,228 t | +1837.5% |
| 2019 | 33,314 t | -27.9% |
| 2020 | 96,041 t | +188.3% |
| 2021 | 3,888 t | -96.0% |
| 2022 | 12,900 t | +231.7% |
| 2023 | 88.39 t | -99.3% |
| 2024 | 2,032 t | +2199.0% |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 13,125 t | 183.78 t | 25,666 t | 8 |
| 2000s | 31,404 t | 32.35 t | 131,693 t | 10 |
| 2010s | 31,300 t | 2,386 t | 72,192 t | 10 |
| 2020s | 22,990 t | 88.39 t | 96,041 t | 5 |
Countries ranked near Belarus
More climate change data for Belarus
- Emissions from livestock — Emissions (CO2eq) 12,124 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 2,377 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 9,748 kt (2050)
- Emissions from livestock — Emissions 8.97 kt (2050)
- Emissions from livestock — Emissions 348.13 kt (2050)
- Emissions from crops — Emissions (CO2eq) 4,092 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 4,078 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 14.36 kt (2050)
- Emissions from crops — Emissions 15.39 kt (2050)
- Emissions from crops — Emissions 0.513 kt (2050)
Frequently asked questions
- What is savanna — burning crop residues in Belarus?
- Savanna — burning crop residues in Belarus was 2,032 t in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest savanna — burning crop residues recorded in Belarus?
- The highest recorded value was 131,693 t in 2002.
- What is the lowest savanna — burning crop residues recorded in Belarus?
- The lowest recorded value was 32.35 t in 2000.
- How does Belarus rank for savanna — burning crop residues?
- Belarus ranks 92nd out of 221 countries with data for 2024.
- Is savanna — burning crop residues rising or falling in Belarus?
- Over the last ten years it is down 97.0%. The long-run trend across the full record is volatile.
- Where does this Belarus 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 — 33 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.