Eswatini vs Sudan (former): Open shrubland — Burning crop residues
Eswatini
17,466 t
in 2024
Sudan (former)
17,126 t
in 2011
Eswatini rank
26th
Sudan (former) rank
27th
Open shrubland — Burning crop residues over time
- Eswatini
- Sudan (former)
How they compare
Eswatini currently reports 17,466 t against 17,126 t in Sudan (former), a difference of 340 t.
The two have swapped places 3 times across 22 shared years of data; in 1990 it was Sudan (former) ahead.
Eswatini ranks 26th and Sudan (former) ranks 27th of 218 countries.
Across the 3 decades both report, Eswatini averaged higher in 1 and Sudan (former) in 2.
Head to head by decade
| Decade | Eswatini | Sudan (former) | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 31,274 t | 6.18 million t | 6.15 million t | Sudan (former) |
| 2000s | 75,689 t | 1.79 million t | 1.72 million t | Sudan (former) |
| 2010s | 72,008 t | 16,820 t | 55,188 t | Eswatini |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher open shrubland — burning crop residues, Eswatini or Sudan (former)?
- Eswatini, at 17,466 t against 17,126 t in Sudan (former) as of 2024.
- What is the difference in open shrubland — burning crop residues between Eswatini and Sudan (former)?
- 340 t, with Eswatini ahead.
- How many years of comparable data are there for Eswatini and Sudan (former)?
- 22 years are reported by both, from 1990 to 2011.
- How do Eswatini and Sudan (former) rank globally for open shrubland — burning crop residues?
- Eswatini ranks 26th and Sudan (former) ranks 27th of 218 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as 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.