Bangladesh vs Southern Asia: Cropland organic soils — Emissions
Bangladesh
2.5 kt
in 2024
Southern Asia
3.87 kt
in 2024
Bangladesh rank
19th
Southern Asia rank
20th
Cropland organic soils — Emissions over time
- Bangladesh
- Southern Asia
How they compare
Southern Asia currently reports 3.87 kt against 2.5 kt in Bangladesh, a difference of 1.37 kt.
That makes Southern Asia's figure about 1.5 times Bangladesh's.
Across all 35 years both countries report, Southern Asia has been ahead every year.
Bangladesh ranks 19th and Southern Asia ranks 20th of 221 countries.
Southern Asia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Bangladesh | Southern Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 2.62 kt | 3.99 kt | 1.37 kt | Southern Asia |
| 2000s | 2.56 kt | 3.98 kt | 1.42 kt | Southern Asia |
| 2010s | 2.54 kt | 3.94 kt | 1.4 kt | Southern Asia |
| 2020s | 2.52 kt | 3.89 kt | 1.37 kt | Southern Asia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Bangladesh or Southern Asia?
- Southern Asia, at 3.87 kt against 2.5 kt in Bangladesh as of 2024.
- What is the difference in cropland organic soils — emissions between Bangladesh and Southern Asia?
- 1.37 kt, with Southern Asia ahead.
- How many years of comparable data are there for Bangladesh and Southern Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Bangladesh and Southern Asia rank globally for cropland organic soils — emissions?
- Bangladesh ranks 19th and Southern Asia ranks 20th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland 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.