Closed shrubland — Emissions in Eastern Asia
Eastern Asia: Closed shrubland — Emissions was 0.0004 kt in 2024. ◆ Volatile
Closed shrubland — Emissions in Eastern 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 Eastern Asia is 0.0004 kt, measured in 2024.
That represents a change of down 90.9% over ten years.
Over the whole period, closed shrubland — emissions in Eastern Asia peaked at 0.1072 kt in 2000 and was at its lowest, 0 kt, in 2003.
Eastern Asia ranks 18th 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.
Closed shrubland — Emissions in Eastern Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 0.0176 kt | — |
| 1991 | 0.0176 kt | +0.0% |
| 1992 | 0.0176 kt | +0.0% |
| 1993 | 0.0176 kt | +0.0% |
| 1994 | 0.0176 kt | +0.0% |
| 1995 | 0.0176 kt | +0.0% |
| 1996 | 0.0845 kt | +380.1% |
| 1997 | 0.1005 kt | +18.9% |
| 1998 | 0.087 kt | -13.4% |
| 1999 | 0.0735 kt | -15.5% |
| 2000 | 0.1072 kt | +45.9% |
| 2001 | 0.0008 kt | -99.3% |
| 2002 | 0.0019 kt | +137.5% |
| 2003 | 0 kt | -100.0% |
| 2004 | 0 kt | — |
| 2005 | 0.003 kt | — |
| 2006 | 0.0014 kt | -53.3% |
| 2007 | 0.0004 kt | -71.4% |
| 2008 | 0.0008 kt | +100.0% |
| 2009 | 0.002 kt | +150.0% |
| 2010 | 0.0025 kt | +25.0% |
| 2011 | 0.0029 kt | +16.0% |
| 2012 | 0.0042 kt | +44.8% |
| 2013 | 0.0065 kt | +54.8% |
| 2014 | 0.0044 kt | -32.3% |
| 2015 | 0.0005 kt | -88.6% |
| 2016 | 0.0006 kt | +20.0% |
| 2017 | 0.002 kt | +233.3% |
| 2018 | 0 kt | -100.0% |
| 2019 | 0.0014 kt | — |
| 2020 | 0.0001 kt | -92.9% |
| 2021 | 0.001 kt | +900.0% |
| 2022 | 0 kt | -100.0% |
| 2023 | 0 kt | — |
| 2024 | 0.0004 kt | — |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.0451 kt | 0.0176 kt | 0.1005 kt | 10 |
| 2000s | 0.0118 kt | 0 kt | 0.1072 kt | 10 |
| 2010s | 0.0025 kt | 0 kt | 0.0065 kt | 10 |
| 2020s | 0.0003 kt | 0 kt | 0.001 kt | 5 |
Countries ranked near Eastern Asia
More climate change data for Eastern Asia
- Emissions from livestock — Emissions (CO2eq) 650,555 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 205,086 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 445,468 kt (2050)
- Emissions from livestock — Emissions 773.91 kt (2050)
- Emissions from livestock — Emissions 15,910 kt (2050)
- Emissions from crops — Emissions (CO2eq) 363,511 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 206,758 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 156,753 kt (2050)
- Emissions from crops — Emissions 780.22 kt (2050)
- Emissions from crops — Emissions 5,598 kt (2050)
Frequently asked questions
- What is closed shrubland — emissions in Eastern Asia?
- Closed shrubland — emissions in Eastern Asia was 0.0004 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest closed shrubland — emissions recorded in Eastern Asia?
- The highest recorded value was 0.1072 kt in 2000.
- What is the lowest closed shrubland — emissions recorded in Eastern Asia?
- The lowest recorded value was 0 kt in 2003.
- How does Eastern Asia rank for closed shrubland — emissions?
- Eastern Asia ranks 18th out of 31 groups with data for 2024.
- Is closed shrubland — emissions rising or falling in Eastern Asia?
- Over the last ten years it is down 90.9%. The long-run trend across the full record is volatile.
- Where does this Eastern 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.