Russian Federation vs Somalia: Closed shrubland — Emissions (N2O)
Russian Federation
0 kt
in 2024
Somalia
0 kt
in 2024
Russian Federation rank
34th
Somalia rank
34th
Closed shrubland — Emissions (N2O) over time
- Russian Federation
- Somalia
How they compare
Russian Federation currently reports 0 kt against 0 kt in Somalia, a difference of 0 kt.
The two have swapped places 7 times across 33 shared years of data; in 1992 it was Russian Federation ahead.
Russian Federation ranks 34th and Somalia ranks 34th of 219 countries.
Russian Federation has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Russian Federation | Somalia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.2027 kt | 0.0059 kt | 0.1968 kt | Russian Federation |
| 2000s | 0.0309 kt | 0.0007 kt | 0.0302 kt | Russian Federation |
| 2010s | 0.0016 kt | 0.001 kt | 0.0006 kt | Russian Federation |
| 2020s | 0.0001 kt | 0 kt | 0.0001 kt | Russian Federation |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — emissions, Russian Federation or Somalia?
- Russian Federation, at 0 kt against 0 kt in Somalia as of 2024.
- What is the difference in closed shrubland — emissions between Russian Federation and Somalia?
- 0 kt, with Russian Federation ahead.
- How many years of comparable data are there for Russian Federation and Somalia?
- 33 years are reported by both, from 1992 to 2024.
- How do Russian Federation and Somalia rank globally for closed shrubland — emissions?
- Russian Federation ranks 34th and Somalia ranks 34th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — 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 Fires consists of estimates of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from biomass burning in a range of vegetation types and from fires in organic soils.