Bangladesh vs Central Asia: Drained organic soils — Emissions (N2O)
Bangladesh
2.73 kt
in 2024
Central Asia
0.0038 kt
in 2024
Bangladesh rank
28th
Central Asia rank
28th
Drained organic soils — Emissions (N2O) over time
- Bangladesh
- Central Asia
How they compare
Bangladesh currently reports 2.73 kt against 0.0038 kt in Central Asia, a difference of 2.73 kt.
That makes Bangladesh's figure about 719.5 times Central Asia's.
Across all 33 years both countries report, Bangladesh has been ahead every year.
Bangladesh ranks 28th and Central Asia ranks 28th of 221 countries.
Bangladesh has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Bangladesh | Central Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 2.85 kt | 0.004 kt | 2.85 kt | Bangladesh |
| 2000s | 2.79 kt | 0.005 kt | 2.79 kt | Bangladesh |
| 2010s | 2.77 kt | 0.0049 kt | 2.77 kt | Bangladesh |
| 2020s | 2.75 kt | 0.0038 kt | 2.75 kt | Bangladesh |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Bangladesh or Central Asia?
- Bangladesh, at 2.73 kt against 0.0038 kt in Central Asia as of 2024.
- What is the difference in drained organic soils — emissions between Bangladesh and Central Asia?
- 2.73 kt, with Bangladesh ahead.
- How many years of comparable data are there for Bangladesh and Central Asia?
- 33 years are reported by both, from 1992 to 2024.
- How do Bangladesh and Central Asia rank globally for drained organic soils — emissions?
- Bangladesh ranks 28th and Central Asia ranks 28th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Drained organic soils — Emissions (N2O). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The FAOSTAT domain on Emissions from drained organic soils consists of nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from the mineralization and oxidation of organic matter in organic soils that are drained for agricultural activities.