Eswatini vs Northern Europe: Open shrubland — Burning crop residues
Eswatini
17,466 t
in 2024
Northern Europe
0 t
in 2024
Eswatini rank
26th
Northern Europe rank
26th
Open shrubland — Burning crop residues over time
- Eswatini
- Northern Europe
How they compare
Eswatini currently reports 17,466 t against 0 t in Northern Europe, a difference of 17,466 t.
The two have swapped places 4 times across 35 shared years of data; in 1990 it was Eswatini ahead.
Eswatini ranks 26th and Northern Europe ranks 26th of 218 countries.
Eswatini has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Eswatini | Northern Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 31,274 t | 12,159 t | 19,115 t | Eswatini |
| 2000s | 75,689 t | 228.04 t | 75,461 t | Eswatini |
| 2010s | 43,419 t | 216.24 t | 43,203 t | Eswatini |
| 2020s | 10,480 t | 308.82 t | 10,171 t | Eswatini |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher open shrubland — burning crop residues, Eswatini or Northern Europe?
- Eswatini, at 17,466 t against 0 t in Northern Europe as of 2024.
- What is the difference in open shrubland — burning crop residues between Eswatini and Northern Europe?
- 17,466 t, with Eswatini ahead.
- How many years of comparable data are there for Eswatini and Northern Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do Eswatini and Northern Europe rank globally for open shrubland — burning crop residues?
- Eswatini ranks 26th and Northern Europe ranks 26th 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.