Closed shrubland — Emissions in Western Asia
Western Asia: Closed shrubland — Emissions was 0 kt in 2024. ◆ Volatile
Closed shrubland — Emissions in Western Asia, 1990–2024
Source: Food and Agriculture Organization of the United Nations. Measured in kt.
Analysis
Western Asia recorded 0 kt for closed shrubland — emissions in 2024. That is the lowest value across all 35 years on record.
The figure is down 100.0% over five years.
Over the whole period, closed shrubland — emissions in Western Asia peaked at 0.3036 kt in 1998 and was at its lowest, 0 kt, in 2003.
That places Western Asia 20th 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 Western Asia, year by year
| Year | kt | Change |
|---|---|---|
| 1990 | 0.0737 kt | — |
| 1991 | 0.0737 kt | +0.0% |
| 1992 | 0.0936 kt | +27.0% |
| 1993 | 0.0936 kt | +0.0% |
| 1994 | 0.0936 kt | +0.0% |
| 1995 | 0.0936 kt | +0.0% |
| 1996 | 0.2605 kt | +178.3% |
| 1997 | 0.2407 kt | -7.6% |
| 1998 | 0.3036 kt | +26.1% |
| 1999 | 0.2331 kt | -23.2% |
| 2000 | 0.2764 kt | +18.6% |
| 2001 | 0.0013 kt | -99.5% |
| 2002 | 0.0013 kt | +0.0% |
| 2003 | 0 kt | -100.0% |
| 2004 | 0.0013 kt | — |
| 2005 | 0 kt | -100.0% |
| 2006 | 0.0013 kt | — |
| 2007 | 0.0066 kt | +407.7% |
| 2008 | 0.0171 kt | +159.1% |
| 2009 | 0 kt | -100.0% |
| 2010 | 0.0013 kt | — |
| 2011 | 0 kt | -100.0% |
| 2012 | 0 kt | — |
| 2013 | 0.0026 kt | — |
| 2014 | 0 kt | -100.0% |
| 2015 | 0 kt | — |
| 2016 | 0 kt | — |
| 2017 | 0 kt | — |
| 2018 | 0 kt | — |
| 2019 | 0.0079 kt | — |
| 2020 | 0 kt | -100.0% |
| 2021 | 0 kt | — |
| 2022 | 0 kt | — |
| 2023 | 0 kt | — |
| 2024 | 0 kt | — |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1990s | 0.156 kt | 0.0737 kt | 0.3036 kt | 10 |
| 2000s | 0.0305 kt | 0 kt | 0.2764 kt | 10 |
| 2010s | 0.0012 kt | 0 kt | 0.0079 kt | 10 |
| 2020s | 0 kt | 0 kt | 0 kt | 5 |
Countries ranked near Western Asia
More climate change data for Western Asia
- Emissions from livestock — Emissions (CO2eq) 99,546 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from N2O 37,104 kt (2050)
- Emissions from livestock — Emissions (CO2eq) from CH4 62,441 kt (2050)
- Emissions from livestock — Emissions 140.02 kt (2050)
- Emissions from livestock — Emissions 2,230 kt (2050)
- Emissions from crops — Emissions (CO2eq) 26,418 kt (2050)
- Emissions from crops — Emissions (CO2eq) from N2O 22,925 kt (2050)
- Emissions from crops — Emissions (CO2eq) from CH4 3,493 kt (2050)
- Emissions from crops — Emissions 86.51 kt (2050)
- Emissions from crops — Emissions 124.75 kt (2050)
Frequently asked questions
- What is closed shrubland — emissions in Western Asia?
- Closed shrubland — emissions in Western Asia was 0 kt in 2024, according to Food and Agriculture Organization of the United Nations.
- What is the highest closed shrubland — emissions recorded in Western Asia?
- The highest recorded value was 0.3036 kt in 1998.
- What is the lowest closed shrubland — emissions recorded in Western Asia?
- The lowest recorded value was 0 kt in 2003.
- How does Western Asia rank for closed shrubland — emissions?
- Western Asia ranks 20th out of 31 groups with data for 2024.
- Where does this Western 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.