Belarus vs Jamaica: Savanna and woody savanna — Burning crop residues
Belarus
5,162 t
in 2024
Jamaica
3,212 t
in 2024
Belarus rank
93rd
Jamaica rank
95th
Savanna and woody savanna — Burning crop residues over time
- Belarus
- Jamaica
How they compare
Belarus currently reports 5,162 t against 3,212 t in Jamaica, a difference of 1,950 t.
That makes Belarus's figure about 1.6 times Jamaica's.
The two have swapped places 6 times across 33 shared years of data; in 1992 it was Belarus ahead.
Belarus ranks 93rd and Jamaica ranks 95th of 221 countries.
Belarus has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Belarus | Jamaica | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 28,771 t | 2,190 t | 26,581 t | Belarus |
| 2000s | 80,018 t | 2,161 t | 77,857 t | Belarus |
| 2010s | 61,271 t | 2,479 t | 58,792 t | Belarus |
| 2020s | 27,897 t | 1,854 t | 26,043 t | Belarus |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna and woody savanna — burning crop residues, Belarus or Jamaica?
- Belarus, at 5,162 t against 3,212 t in Jamaica as of 2024.
- What is the difference in savanna and woody savanna — burning crop residues between Belarus and Jamaica?
- 1,950 t, with Belarus ahead.
- How many years of comparable data are there for Belarus and Jamaica?
- 33 years are reported by both, from 1992 to 2024.
- How do Belarus and Jamaica rank globally for savanna and woody savanna — burning crop residues?
- Belarus ranks 93rd and Jamaica ranks 95th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Savanna and woody savanna — 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.