Russian Federation vs South Sudan: Closed shrubland — Burning crop residues
Russian Federation
0 t
in 2024
South Sudan
0 t
in 2024
Russian Federation rank
34th
South Sudan rank
34th
Closed shrubland — Burning crop residues over time
- Russian Federation
- South Sudan
How they compare
Russian Federation currently reports 0 t against 0 t in South Sudan, a difference of 0 t.
The two have swapped places 3 times across 13 shared years of data; in 2012 it was Russian Federation ahead.
Russian Federation ranks 34th and South Sudan ranks 34th of 219 countries.
Russian Federation has averaged higher in every one of the 2 decades both report.
Head to head by decade
| Decade | Russian Federation | South Sudan | Difference | Ahead |
|---|---|---|---|---|
| 2010s | 8,714 t | 71.33 t | 8,643 t | Russian Federation |
| 2020s | 691.61 t | 0 t | 691.61 t | Russian Federation |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Russian Federation or South Sudan?
- Russian Federation, at 0 t against 0 t in South Sudan as of 2024.
- What is the difference in closed shrubland — burning crop residues between Russian Federation and South Sudan?
- 0 t, with Russian Federation ahead.
- How many years of comparable data are there for Russian Federation and South Sudan?
- 13 years are reported by both, from 2012 to 2024.
- How do Russian Federation and South Sudan rank globally for closed shrubland — burning crop residues?
- Russian Federation ranks 34th and South Sudan ranks 34th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — Burning crop residues (Biomass burned, dry matter). 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.