Cambodia vs Russian Federation: Closed shrubland — Emissions (N2O)
Cambodia
0 kt
in 2024
Russian Federation
0 kt
in 2024
Cambodia rank
34th
Russian Federation rank
34th
Closed shrubland — Emissions (N2O) over time
- Cambodia
- Russian Federation
How they compare
Cambodia currently reports 0 kt against 0 kt in Russian Federation, a difference of 0 kt.
The two have swapped places 14 times across 33 shared years of data; in 1992 it was Russian Federation ahead.
Cambodia ranks 34th and Russian Federation ranks 34th of 219 countries.
Across the 4 decades both report, Cambodia averaged higher in 2 and Russian Federation in 2.
Head to head by decade
| Decade | Cambodia | Russian Federation | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.0323 kt | 0.2027 kt | 0.1704 kt | Russian Federation |
| 2000s | 0.0032 kt | 0.0309 kt | 0.0277 kt | Russian Federation |
| 2010s | 0.002 kt | 0.0016 kt | 0.0004 kt | Cambodia |
| 2020s | 0.0006 kt | 0.0001 kt | 0.0005 kt | Cambodia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — emissions, Cambodia or Russian Federation?
- Cambodia, at 0 kt against 0 kt in Russian Federation as of 2024.
- What is the difference in closed shrubland — emissions between Cambodia and Russian Federation?
- 0 kt, with Cambodia ahead.
- How many years of comparable data are there for Cambodia and Russian Federation?
- 33 years are reported by both, from 1992 to 2024.
- How do Cambodia and Russian Federation rank globally for closed shrubland — emissions?
- Cambodia ranks 34th and Russian Federation 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.