Closed shrubland — Emissions in Southern Asia
Southern Asia: Closed shrubland — Emissions was 0.0001 kt in 2024. ◆ Volatile
Closed shrubland — Emissions in Southern Asia, 1990–2024
Source: Food and Agriculture Organization of the United Nations. Measured in kt.
Analysis
Southern Asia recorded 0.0001 kt for closed shrubland — emissions in 2024.
The figure is unchanged over ten years.
Over the whole period, closed shrubland — emissions in Southern Asia peaked at 0.0719 kt in 1999 and was at its lowest, 0 kt, in 2002.
That places Southern Asia 19th out of 31 groups 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.
Closed shrubland — Emissions in Southern Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 0.0126 kt | — |
| 1991 | 0.0126 kt | +0.0% |
| 1992 | 0.0126 kt | +0.0% |
| 1993 | 0.0126 kt | +0.0% |
| 1994 | 0.0126 kt | +0.0% |
| 1995 | 0.0126 kt | +0.0% |
| 1996 | 0.0677 kt | +437.3% |
| 1997 | 0.0295 kt | -56.4% |
| 1998 | 0.0484 kt | +64.1% |
| 1999 | 0.0719 kt | +48.6% |
| 2000 | 0.0464 kt | -35.5% |
| 2001 | 0.0005 kt | -98.9% |
| 2002 | 0 kt | -100.0% |
| 2003 | 0.0001 kt | — |
| 2004 | 0.0001 kt | +0.0% |
| 2005 | 0 kt | -100.0% |
| 2006 | 0 kt | — |
| 2007 | 0 kt | — |
| 2008 | 0 kt | — |
| 2009 | 0.0002 kt | — |
| 2010 | 0 kt | -100.0% |
| 2011 | 0 kt | — |
| 2012 | 0 kt | — |
| 2013 | 0 kt | — |
| 2014 | 0.0001 kt | — |
| 2015 | 0 kt | -100.0% |
| 2016 | 0 kt | — |
| 2017 | 0 kt | — |
| 2018 | 0 kt | — |
| 2019 | 0 kt | — |
| 2020 | 0 kt | — |
| 2021 | 0 kt | — |
| 2022 | 0.0001 kt | — |
| 2023 | 0 kt | -100.0% |
| 2024 | 0.0001 kt | — |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.0293 kt | 0.0126 kt | 0.0719 kt | 10 |
| 2000s | 0.0047 kt | 0 kt | 0.0464 kt | 10 |
| 2010s | 0 kt | 0 kt | 0.0001 kt | 10 |
| 2020s | 0 kt | 0 kt | 0.0001 kt | 5 |
Countries ranked near Southern Asia
More climate change data for Southern Asia
- Emissions from livestock — Emissions (CO2eq) 933,596 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 178,099 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 755,497 kt (2050)
- Emissions from livestock — Emissions 672.07 kt (2050)
- Emissions from livestock — Emissions 26,982 kt (2050)
- Emissions from crops — Emissions (CO2eq) 403,904 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 246,070 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 157,834 kt (2050)
- Emissions from crops — Emissions 928.57 kt (2050)
- Emissions from crops — Emissions 5,637 kt (2050)
Frequently asked questions
- What is closed shrubland — emissions in Southern Asia?
- Closed shrubland — emissions in Southern Asia was 0.0001 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest closed shrubland — emissions recorded in Southern Asia?
- The highest recorded value was 0.0719 kt in 1999.
- What is the lowest closed shrubland — emissions recorded in Southern Asia?
- The lowest recorded value was 0 kt in 2002.
- How does Southern Asia rank for closed shrubland — emissions?
- Southern Asia ranks 19th out of 31 groups with data for 2024.
- Is closed shrubland — emissions rising or falling in Southern Asia?
- Over the last ten years it is unchanged. The long-run trend across the full record is volatile.
- Where does this Southern 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.