Guatemala vs Northern Europe: Other forest — Burning crop residues
Guatemala
433,390 t
in 2024
Northern Europe
0 t
in 2024
Guatemala rank
29th
Northern Europe rank
29th
Other forest — Burning crop residues over time
- Guatemala
- Northern Europe
How they compare
Guatemala currently reports 433,390 t against 0 t in Northern Europe, a difference of 433,390 t.
The two have swapped places 10 times across 35 shared years of data; in 1990 it was Guatemala ahead.
Guatemala ranks 29th and Northern Europe ranks 29th of 219 countries.
Guatemala has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Guatemala | Northern Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 121,649 t | 62,624 t | 59,025 t | Guatemala |
| 2000s | 74,936 t | 62,317 t | 12,620 t | Guatemala |
| 2010s | 86,783 t | 61,983 t | 24,799 t | Guatemala |
| 2020s | 157,182 t | 5,369 t | 151,813 t | Guatemala |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher other forest — burning crop residues, Guatemala or Northern Europe?
- Guatemala, at 433,390 t against 0 t in Northern Europe as of 2024.
- What is the difference in other forest — burning crop residues between Guatemala and Northern Europe?
- 433,390 t, with Guatemala ahead.
- How many years of comparable data are there for Guatemala and Northern Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do Guatemala and Northern Europe rank globally for other forest — burning crop residues?
- Guatemala ranks 29th and Northern Europe ranks 29th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Other forest — 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.