Eastern Asia vs Myanmar: Drained organic soils — Emissions (CO2)
Eastern Asia
30,540 kt
in 2024
Myanmar
14,024 kt
in 2024
Eastern Asia rank
18th
Myanmar rank
16th
Drained organic soils — Emissions (CO2) over time
- Eastern Asia
- Myanmar
How they compare
Eastern Asia currently reports 30,540 kt against 14,024 kt in Myanmar, a difference of 16,516 kt.
That makes Eastern Asia's figure about 2.2 times Myanmar's.
Across all 35 years both countries report, Eastern Asia has been ahead every year.
Eastern Asia ranks 18th and Myanmar ranks 16th of 31 groups.
Eastern Asia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Eastern Asia | Myanmar | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 31,457 kt | 14,200 kt | 17,257 kt | Eastern Asia |
| 2000s | 31,473 kt | 14,171 kt | 17,302 kt | Eastern Asia |
| 2010s | 30,888 kt | 14,132 kt | 16,755 kt | Eastern Asia |
| 2020s | 30,570 kt | 14,043 kt | 16,528 kt | Eastern Asia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Eastern Asia or Myanmar?
- Eastern Asia, at 30,540 kt against 14,024 kt in Myanmar as of 2024.
- What is the difference in drained organic soils — emissions between Eastern Asia and Myanmar?
- 16,516 kt, with Eastern Asia ahead.
- How many years of comparable data are there for Eastern Asia and Myanmar?
- 35 years are reported by both, from 1990 to 2024.
- How do Eastern Asia and Myanmar rank globally for drained organic soils — emissions?
- Eastern Asia ranks 18th and Myanmar ranks 16th of 31 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Drained organic soils — Emissions (CO2). 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.