Estonia vs Western Africa: Cropland organic soils — Emissions
Estonia
4,528 kt
in 2024
Western Africa
3,133 kt
in 2024
Estonia rank
22nd
Western Africa rank
22nd
Cropland organic soils — Emissions over time
- Estonia
- Western Africa
How they compare
Estonia currently reports 4,528 kt against 3,133 kt in Western Africa, a difference of 1,395 kt.
That makes Estonia's figure about 1.4 times Western Africa's.
Across all 33 years both countries report, Estonia has been ahead every year.
Estonia ranks 22nd and Western Africa ranks 22nd of 221 countries.
Estonia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Estonia | Western Africa | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 3,646 kt | 2,912 kt | 734.36 kt | Estonia |
| 2000s | 4,341 kt | 3,096 kt | 1,245 kt | Estonia |
| 2010s | 4,516 kt | 3,118 kt | 1,398 kt | Estonia |
| 2020s | 4,525 kt | 3,135 kt | 1,391 kt | Estonia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Estonia or Western Africa?
- Estonia, at 4,528 kt against 3,133 kt in Western Africa as of 2024.
- What is the difference in cropland organic soils — emissions between Estonia and Western Africa?
- 1,395 kt, with Estonia ahead.
- How many years of comparable data are there for Estonia and Western Africa?
- 33 years are reported by both, from 1992 to 2024.
- How do Estonia and Western Africa rank globally for cropland organic soils — emissions?
- Estonia ranks 22nd and Western Africa ranks 22nd of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland 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.