Cropland organic soils — Emissions in Eastern Africa
Eastern Africa: Cropland organic soils — Emissions was 5.04 kt in 2024. ▲ Rising
Cropland organic soils — Emissions in Eastern Africa, 1990–2024
Source: Food and Agriculture Organization of the United Nations. Measured in kt.
Analysis
The most recent figure for cropland organic soils — emissions in Eastern Africa is 5.04 kt, measured in 2024.
The figure is down 1.8% over ten years.
Over the whole period, cropland organic soils — emissions in Eastern Africa peaked at 5.15 kt in 2012 and was at its lowest, 4.8 kt, in 1994.
That places Eastern Africa 19th out of 31 groups with data for 2024, putting it in the middle of the range.
The long-run direction has been consistently rising across the 35 years of available data.
Cropland organic soils — Emissions in Eastern Africa, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 4.8 kt | — |
| 1991 | 4.8 kt | +0.0% |
| 1992 | 4.8 kt | +0.0% |
| 1993 | 4.8 kt | -0.0% |
| 1994 | 4.8 kt | -0.0% |
| 1995 | 4.85 kt | +0.9% |
| 1996 | 4.85 kt | +0.1% |
| 1997 | 4.86 kt | +0.1% |
| 1998 | 4.87 kt | +0.3% |
| 1999 | 4.9 kt | +0.6% |
| 2000 | 4.9 kt | +0.0% |
| 2001 | 4.9 kt | +0.0% |
| 2002 | 4.91 kt | +0.2% |
| 2003 | 4.9 kt | -0.1% |
| 2004 | 4.9 kt | +0.0% |
| 2005 | 4.91 kt | +0.1% |
| 2006 | 4.91 kt | +0.0% |
| 2007 | 4.91 kt | -0.1% |
| 2008 | 4.91 kt | +0.0% |
| 2009 | 4.91 kt | +0.1% |
| 2010 | 4.91 kt | +0.0% |
| 2011 | 4.91 kt | +0.0% |
| 2012 | 5.15 kt | +4.9% |
| 2013 | 5.14 kt | -0.3% |
| 2014 | 5.13 kt | -0.2% |
| 2015 | 5.13 kt | -0.0% |
| 2016 | 5.09 kt | -0.7% |
| 2017 | 5.09 kt | -0.2% |
| 2018 | 5.07 kt | -0.2% |
| 2019 | 5.06 kt | -0.2% |
| 2020 | 5.07 kt | +0.0% |
| 2021 | 5.05 kt | -0.4% |
| 2022 | 5.04 kt | -0.1% |
| 2023 | 5.04 kt | +0.0% |
| 2024 | 5.04 kt | +0.0% |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 4.83 kt | 4.8 kt | 4.9 kt | 10 |
| 2000s | 4.9 kt | 4.9 kt | 4.91 kt | 10 |
| 2010s | 5.07 kt | 4.91 kt | 5.15 kt | 10 |
| 2020s | 5.04 kt | 5.04 kt | 5.07 kt | 5 |
Countries ranked near Eastern Africa
More climate change data for Eastern Africa
- Emissions from livestock — Emissions (CO2eq) 337,539 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 111,806 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 225,733 kt (2050)
- Emissions from livestock — Emissions 421.91 kt (2050)
- Emissions from livestock — Emissions 8,062 kt (2050)
- Emissions from crops — Emissions (CO2eq) 36,052 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 19,110 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 16,942 kt (2050)
- Emissions from crops — Emissions 72.11 kt (2050)
- Emissions from crops — Emissions 605.08 kt (2050)
Frequently asked questions
- What is cropland organic soils — emissions in Eastern Africa?
- Cropland organic soils — emissions in Eastern Africa was 5.04 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest cropland organic soils — emissions recorded in Eastern Africa?
- The highest recorded value was 5.15 kt in 2012.
- What is the lowest cropland organic soils — emissions recorded in Eastern Africa?
- The lowest recorded value was 4.8 kt in 1994.
- How does Eastern Africa rank for cropland organic soils — emissions?
- Eastern Africa ranks 19th out of 31 groups with data for 2024.
- Is cropland organic soils — emissions rising or falling in Eastern Africa?
- Over the last ten years it is down 1.8%. The long-run trend across the full record is rising.
- Where does this Eastern Africa data come from?
- The figures come from Food and Agriculture Organization of the United Nations, published as part of Cropland organic soils — Emissions (N2O). 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 drained organic soils consists of nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from the mineralization and oxidation of organic matter in organic soils that are drained for agricultural activities.