Iceland vs Northern Africa: Grassland organic soils — Emissions
Iceland
0.525 kt
in 2024
Northern Africa
0 kt
in 2024
Iceland rank
27th
Northern Africa rank
29th
Grassland organic soils — Emissions over time
- Iceland
- Northern Africa
How they compare
Iceland currently reports 0.525 kt against 0 kt in Northern Africa, a difference of 0.525 kt.
The two have swapped places 1 time across 35 shared years of data; in 1990 it was Northern Africa ahead.
Iceland ranks 27th and Northern Africa ranks 29th of 221 countries.
Across the 4 decades both report, Iceland averaged higher in 2 and Northern Africa in 2.
Head to head by decade
| Decade | Iceland | Northern Africa | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.5222 kt | 1.82 kt | 1.29 kt | Northern Africa |
| 2000s | 0.5221 kt | 1.81 kt | 1.29 kt | Northern Africa |
| 2010s | 0.5224 kt | 0.3614 kt | 0.161 kt | Iceland |
| 2020s | 0.525 kt | 0 kt | 0.525 kt | Iceland |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — emissions, Iceland or Northern Africa?
- Iceland, at 0.525 kt against 0 kt in Northern Africa as of 2024.
- What is the difference in grassland organic soils — emissions between Iceland and Northern Africa?
- 0.525 kt, with Iceland ahead.
- How many years of comparable data are there for Iceland and Northern Africa?
- 35 years are reported by both, from 1990 to 2024.
- How do Iceland and Northern Africa rank globally for grassland organic soils — emissions?
- Iceland ranks 27th and Northern Africa ranks 29th 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.