China vs Southern Europe: Grassland organic soils — Emissions
China
0.8838 kt
in 2024
Southern Europe
0.1602 kt
in 2024
China rank
22nd
Southern Europe rank
22nd
Grassland organic soils — Emissions over time
- China
- Southern Europe
How they compare
China currently reports 0.8838 kt against 0.1602 kt in Southern Europe, a difference of 0.7236 kt.
That makes China's figure about 5.5 times Southern Europe's.
Across all 35 years both countries report, China has been ahead every year.
China ranks 22nd and Southern Europe ranks 22nd of 221 countries.
China has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | China | Southern Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.8708 kt | 0.1478 kt | 0.723 kt | China |
| 2000s | 0.8728 kt | 0.1629 kt | 0.7098 kt | China |
| 2010s | 0.8745 kt | 0.1631 kt | 0.7114 kt | China |
| 2020s | 0.8838 kt | 0.1602 kt | 0.7236 kt | China |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — emissions, China or Southern Europe?
- China, at 0.8838 kt against 0.1602 kt in Southern Europe as of 2024.
- What is the difference in grassland organic soils — emissions between China and Southern Europe?
- 0.7236 kt, with China ahead.
- How many years of comparable data are there for China and Southern Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do China and Southern Europe rank globally for grassland organic soils — emissions?
- China ranks 22nd and Southern Europe ranks 22nd of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland 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.