Closed shrubland — Emissions in Asia
Asia: Closed shrubland — Emissions was 0.004 kt in 2024. ◆ Volatile
Closed shrubland — Emissions in Asia, 1990–2024
Source: Food and Agriculture Organization of the United Nations. Measured in kt.
Analysis
The most recent figure for closed shrubland — emissions in Asia is 0.004 kt, measured in 2024.
The figure is up 33.3% on the previous year and down 71.8% over ten years.
Over the whole period, closed shrubland — emissions in Asia peaked at 0.6199 kt in 1998 and was at its lowest, 0.0007 kt, in 2022.
That places Asia 4th out of 21 regions with data for 2024, putting it in the top quarter.
The series is highly variable year to year, so single readings are best treated with caution.
Closed shrubland — Emissions in Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 0.0606 kt | — |
| 1991 | 0.0606 kt | +0.0% |
| 1992 | 0.1209 kt | +99.5% |
| 1993 | 0.1209 kt | +0.0% |
| 1994 | 0.1209 kt | +0.0% |
| 1995 | 0.1209 kt | +0.0% |
| 1996 | 0.6197 kt | +412.6% |
| 1997 | 0.5696 kt | -8.1% |
| 1998 | 0.6199 kt | +8.8% |
| 1999 | 0.549 kt | -11.4% |
| 2000 | 0.5161 kt | -6.0% |
| 2001 | 0.01 kt | -98.1% |
| 2002 | 0.0049 kt | -51.0% |
| 2003 | 0.0052 kt | +6.1% |
| 2004 | 0.0025 kt | -51.9% |
| 2005 | 0.008 kt | +220.0% |
| 2006 | 0.004 kt | -50.0% |
| 2007 | 0.0054 kt | +35.0% |
| 2008 | 0.0043 kt | -20.4% |
| 2009 | 0.007 kt | +62.8% |
| 2010 | 0.0072 kt | +2.9% |
| 2011 | 0.0094 kt | +30.6% |
| 2012 | 0.0074 kt | -21.3% |
| 2013 | 0.0142 kt | +91.9% |
| 2014 | 0.0142 kt | +0.0% |
| 2015 | 0.0091 kt | -35.9% |
| 2016 | 0.0038 kt | -58.2% |
| 2017 | 0.0028 kt | -26.3% |
| 2018 | 0.0018 kt | -35.7% |
| 2019 | 0.0047 kt | +161.1% |
| 2020 | 0.0014 kt | -70.2% |
| 2021 | 0.0062 kt | +342.9% |
| 2022 | 0.0007 kt | -88.7% |
| 2023 | 0.003 kt | +328.6% |
| 2024 | 0.004 kt | +33.3% |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.2963 kt | 0.0606 kt | 0.6199 kt | 10 |
| 2000s | 0.0567 kt | 0.0025 kt | 0.5161 kt | 10 |
| 2010s | 0.0075 kt | 0.0018 kt | 0.0142 kt | 10 |
| 2020s | 0.0031 kt | 0.0007 kt | 0.0062 kt | 5 |
Countries ranked near Asia
More climate change data for Asia
- Emissions from livestock — Emissions (CO2eq) 2.01 million kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 512,601 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 1.49 million kt (2050)
- Emissions from livestock — Emissions 1,934 kt (2050)
- Emissions from livestock — Emissions 53,345 kt (2050)
- Emissions from crops — Emissions (CO2eq) 1.12 million kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 552,825 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 567,748 kt (2050)
- Emissions from crops — Emissions 2,086 kt (2050)
- Emissions from crops — Emissions 20,277 kt (2050)
Frequently asked questions
- What is closed shrubland — emissions in Asia?
- Closed shrubland — emissions in Asia was 0.004 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest closed shrubland — emissions recorded in Asia?
- The highest recorded value was 0.6199 kt in 1998.
- What is the lowest closed shrubland — emissions recorded in Asia?
- The lowest recorded value was 0.0007 kt in 2022.
- How does Asia rank for closed shrubland — emissions?
- Asia ranks 4th out of 21 regions with data for 2024.
- Is closed shrubland — emissions rising or falling in Asia?
- Over the last ten years it is down 71.8%. The long-run trend across the full record is volatile.
- Where does this Asia data come from?
- The figures come from Food and Agriculture Organization of the United Nations, published as part of Closed shrubland — 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 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.