Closed shrubland — Emissions in Eastern Asia
Eastern Asia: Closed shrubland — Emissions was 0.004 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
Eastern Asia recorded 0.004 kt for closed shrubland — emissions in 2024.
That represents a change of down 91.8% over ten years.
Over the whole period, closed shrubland — emissions in Eastern Asia peaked at 1.17 kt in 2000 and was at its lowest, 0 kt, in 2003.
That places Eastern Asia 18th 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 Eastern Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 0.1931 kt | — |
| 1991 | 0.1931 kt | +0.0% |
| 1992 | 0.1931 kt | +0.0% |
| 1993 | 0.1931 kt | +0.0% |
| 1994 | 0.1931 kt | +0.0% |
| 1995 | 0.1931 kt | +0.0% |
| 1996 | 0.9253 kt | +379.2% |
| 1997 | 1.1 kt | +19.0% |
| 1998 | 0.9528 kt | -13.5% |
| 1999 | 0.8049 kt | -15.5% |
| 2000 | 1.17 kt | +45.9% |
| 2001 | 0.0092 kt | -99.2% |
| 2002 | 0.0211 kt | +129.3% |
| 2003 | 0 kt | -100.0% |
| 2004 | 0 kt | — |
| 2005 | 0.033 kt | — |
| 2006 | 0.0158 kt | -52.1% |
| 2007 | 0.004 kt | -74.7% |
| 2008 | 0.0092 kt | +130.0% |
| 2009 | 0.0224 kt | +143.5% |
| 2010 | 0.0276 kt | +23.2% |
| 2011 | 0.0316 kt | +14.5% |
| 2012 | 0.0461 kt | +45.9% |
| 2013 | 0.0711 kt | +54.2% |
| 2014 | 0.0487 kt | -31.5% |
| 2015 | 0.0053 kt | -89.1% |
| 2016 | 0.0066 kt | +24.5% |
| 2017 | 0.0224 kt | +239.4% |
| 2018 | 0 kt | -100.0% |
| 2019 | 0.0158 kt | — |
| 2020 | 0.0013 kt | -91.8% |
| 2021 | 0.0106 kt | +715.4% |
| 2022 | 0 kt | -100.0% |
| 2023 | 0 kt | — |
| 2024 | 0.004 kt | — |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.4943 kt | 0.1931 kt | 1.1 kt | 10 |
| 2000s | 0.1289 kt | 0 kt | 1.17 kt | 10 |
| 2010s | 0.0275 kt | 0 kt | 0.0711 kt | 10 |
| 2020s | 0.0032 kt | 0 kt | 0.0106 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 0.004 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 1.17 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 91.8%. 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 (CH4). 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.