Myanmar vs Southern Europe: Cropland organic soils — Emissions
Myanmar
1.94 kt
in 2024
Southern Europe
1.83 kt
in 2024
Myanmar rank
22nd
Southern Europe rank
21st
Cropland organic soils — Emissions over time
- Myanmar
- Southern Europe
How they compare
Myanmar currently reports 1.94 kt against 1.83 kt in Southern Europe, a difference of 0.11 kt.
That makes Myanmar's figure about 1.1 times Southern Europe's.
Across all 35 years both countries report, Myanmar has been ahead every year.
Myanmar ranks 22nd and Southern Europe ranks 21st of 221 countries.
Myanmar has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Myanmar | Southern Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.94 kt | 1.83 kt | 0.1096 kt | Myanmar |
| 2000s | 1.95 kt | 1.89 kt | 0.0646 kt | Myanmar |
| 2010s | 1.95 kt | 1.87 kt | 0.0808 kt | Myanmar |
| 2020s | 1.94 kt | 1.83 kt | 0.1116 kt | Myanmar |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Myanmar or Southern Europe?
- Myanmar, at 1.94 kt against 1.83 kt in Southern Europe as of 2024.
- What is the difference in cropland organic soils — emissions between Myanmar and Southern Europe?
- 0.11 kt, with Myanmar ahead.
- How many years of comparable data are there for Myanmar and Southern Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do Myanmar and Southern Europe rank globally for cropland organic soils — emissions?
- Myanmar ranks 22nd and Southern Europe ranks 21st 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.