Belarus vs Papua New Guinea: Closed shrubland — Burning crop residues
Belarus
0 t
in 2024
Papua New Guinea
0 t
in 2024
Belarus rank
34th
Papua New Guinea rank
34th
Closed shrubland — Burning crop residues over time
- Belarus
- Papua New Guinea
How they compare
Belarus currently reports 0 t against 0 t in Papua New Guinea, a difference of 0 t.
Across all 33 years both countries report, Papua New Guinea has been ahead every year.
Belarus ranks 34th and Papua New Guinea ranks 34th of 219 countries.
Papua New Guinea has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Belarus | Papua New Guinea | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 2,342 t | 47,229 t | 44,887 t | Papua New Guinea |
| 2000s | 132.66 t | 3,085 t | 2,952 t | Papua New Guinea |
| 2010s | 0 t | 1,141 t | 1,141 t | Papua New Guinea |
| 2020s | 0 t | 114.15 t | 114.15 t | Papua New Guinea |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Belarus or Papua New Guinea?
- Belarus, at 0 t against 0 t in Papua New Guinea as of 2024.
- What is the difference in closed shrubland — burning crop residues between Belarus and Papua New Guinea?
- 0 t, with Belarus ahead.
- How many years of comparable data are there for Belarus and Papua New Guinea?
- 33 years are reported by both, from 1992 to 2024.
- How do Belarus and Papua New Guinea rank globally for closed shrubland — burning crop residues?
- Belarus ranks 34th and Papua New Guinea 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.