Southern Europe vs Sudan: Closed and open shrubland — Burning crop residues
Southern Europe
16,890 t
in 2024
Sudan
149,866 t
in 2024
Southern Europe rank
23rd
Sudan rank
20th
Closed and open shrubland — Burning crop residues over time
- Southern Europe
- Sudan
How they compare
Sudan currently reports 149,866 t against 16,890 t in Southern Europe, a difference of 132,976 t.
That makes Sudan's figure about 8.9 times Southern Europe's.
The two have swapped places 5 times across 13 shared years of data; in 2012 it was Southern Europe ahead.
Southern Europe ranks 23rd and Sudan ranks 20th of 31 groups.
Across the 2 decades both report, Southern Europe averaged higher in 1 and Sudan in 1.
Head to head by decade
| Decade | Southern Europe | Sudan | Difference | Ahead |
|---|---|---|---|---|
| 2010s | 82,107 t | 26,264 t | 55,843 t | Southern Europe |
| 2020s | 47,046 t | 63,007 t | 15,961 t | Sudan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Southern Europe or Sudan?
- Sudan, at 149,866 t against 16,890 t in Southern Europe as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Southern Europe and Sudan?
- 132,976 t, with Sudan ahead.
- How many years of comparable data are there for Southern Europe and Sudan?
- 13 years are reported by both, from 2012 to 2024.
- How do Southern Europe and Sudan rank globally for closed and open shrubland — burning crop residues?
- Southern Europe ranks 23rd and Sudan ranks 20th of 31 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed and open 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.