Kazakhstan vs Sudan (former): Closed shrubland — Burning crop residues
Kazakhstan
0 t
in 2024
Sudan (former)
0 t
in 2011
Kazakhstan rank
34th
Sudan (former) rank
34th
Closed shrubland — Burning crop residues over time
- Kazakhstan
- Sudan (former)
How they compare
Kazakhstan currently reports 0 t against 0 t in Sudan (former), a difference of 0 t.
The two have swapped places 4 times across 20 shared years of data; in 1992 it was Kazakhstan ahead.
Kazakhstan ranks 34th and Sudan (former) ranks 34th of 219 countries.
Across the 3 decades both report, Kazakhstan averaged higher in 1 and Sudan (former) in 2.
Head to head by decade
| Decade | Kazakhstan | Sudan (former) | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 801,078 t | 5.38 million t | 4.58 million t | Sudan (former) |
| 2000s | 116,688 t | 900,468 t | 783,780 t | Sudan (former) |
| 2010s | 4,313 t | 0 t | 4,313 t | Kazakhstan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Kazakhstan or Sudan (former)?
- Kazakhstan, at 0 t against 0 t in Sudan (former) as of 2024.
- What is the difference in closed shrubland — burning crop residues between Kazakhstan and Sudan (former)?
- 0 t, with Kazakhstan ahead.
- How many years of comparable data are there for Kazakhstan and Sudan (former)?
- 20 years are reported by both, from 1992 to 2011.
- How do Kazakhstan and Sudan (former) rank globally for closed shrubland — burning crop residues?
- Kazakhstan ranks 34th and Sudan (former) 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.