Open shrubland — Emissions in Central Asia
Central Asia: Open shrubland — Emissions was 0.0078 kt in 2024. ◆ Volatile
Open shrubland — Emissions in Central Asia, 1992–2024
Source: Food and Agriculture Organization of the United Nations. Measured in kt.
Analysis
The most recent figure for open shrubland — emissions in Central Asia is 0.0078 kt, measured in 2024.
That represents a change of up 333.3% on the previous year and down 89.7% over ten years.
Over the whole period, open shrubland — emissions in Central Asia peaked at 0.7269 kt in 1997 and was at its lowest, 0.0018 kt, in 2023.
Central Asia ranks 22nd of 31 groups 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.
Open shrubland — Emissions in Central Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1992 | 0.0977 kt | — |
| 1993 | 0.0977 kt | +0.0% |
| 1994 | 0.0977 kt | +0.0% |
| 1995 | 0.0977 kt | +0.0% |
| 1996 | 0.381 kt | +290.0% |
| 1997 | 0.7269 kt | +90.8% |
| 1998 | 0.4929 kt | -32.2% |
| 1999 | 0.3647 kt | -26.0% |
| 2000 | 0.2733 kt | -25.1% |
| 2001 | 0.0174 kt | -93.6% |
| 2002 | 0.005 kt | -71.3% |
| 2003 | 0.0213 kt | +326.0% |
| 2004 | 0.0604 kt | +183.6% |
| 2005 | 0.0731 kt | +21.0% |
| 2006 | 0.0125 kt | -82.9% |
| 2007 | 0.0091 kt | -27.2% |
| 2008 | 0.0061 kt | -33.0% |
| 2009 | 0.0104 kt | +70.5% |
| 2010 | 0.0057 kt | -45.2% |
| 2011 | 0.0112 kt | +96.5% |
| 2012 | 0.023 kt | +105.4% |
| 2013 | 0.0287 kt | +24.8% |
| 2014 | 0.0756 kt | +163.4% |
| 2015 | 0.005 kt | -93.4% |
| 2016 | 0.0068 kt | +36.0% |
| 2017 | 0.023 kt | +238.2% |
| 2018 | 0.0084 kt | -63.5% |
| 2019 | 0.066 kt | +685.7% |
| 2020 | 0.0944 kt | +43.0% |
| 2021 | 0.015 kt | -84.1% |
| 2022 | 0.0059 kt | -60.7% |
| 2023 | 0.0018 kt | -69.5% |
| 2024 | 0.0078 kt | +333.3% |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.2945 kt | 0.0977 kt | 0.7269 kt | 8 |
| 2000s | 0.0489 kt | 0.005 kt | 0.2733 kt | 10 |
| 2010s | 0.0253 kt | 0.005 kt | 0.0756 kt | 10 |
| 2020s | 0.025 kt | 0.0018 kt | 0.0944 kt | 5 |
Countries ranked near Central Asia
More climate change data for Central Asia
- Emissions from livestock — Emissions (CO2eq) 65,233 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 15,658 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 49,576 kt (2050)
- Emissions from livestock — Emissions 59.09 kt (2050)
- Emissions from livestock — Emissions 1,771 kt (2050)
- Emissions from crops — Emissions (CO2eq) 11,927 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 10,307 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 1,620 kt (2050)
- Emissions from crops — Emissions 38.9 kt (2050)
- Emissions from crops — Emissions 57.85 kt (2050)
Frequently asked questions
- What is open shrubland — emissions in Central Asia?
- Open shrubland — emissions in Central Asia was 0.0078 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest open shrubland — emissions recorded in Central Asia?
- The highest recorded value was 0.7269 kt in 1997.
- What is the lowest open shrubland — emissions recorded in Central Asia?
- The lowest recorded value was 0.0018 kt in 2023.
- How does Central Asia rank for open shrubland — emissions?
- Central Asia ranks 22nd out of 31 groups with data for 2024.
- Is open shrubland — emissions rising or falling in Central Asia?
- Over the last ten years it is down 89.7%. The long-run trend across the full record is volatile.
- Where does this Central Asia data come from?
- The figures come from Food and Agriculture Organization of the United Nations, published as part of Open shrubland — Emissions (N2O). 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.