Estonia vs New Caledonia: Grassland — Burning crop residues
Estonia
1,150 t
in 2024
New Caledonia
1,090 t
in 2024
Estonia rank
113th
New Caledonia rank
114th
Grassland — Burning crop residues over time
- Estonia
- New Caledonia
How they compare
Estonia currently reports 1,150 t against 1,090 t in New Caledonia, a difference of 60 t.
That makes Estonia's figure about 1.1 times New Caledonia's.
The two have swapped places 14 times across 33 shared years of data; in 1992 it was Estonia ahead.
Estonia ranks 113th and New Caledonia ranks 114th of 220 countries.
Across the 4 decades both report, Estonia averaged higher in 2 and New Caledonia in 2.
Head to head by decade
| Decade | Estonia | New Caledonia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 523.72 t | 679.46 t | 155.75 t | New Caledonia |
| 2000s | 1,675 t | 575.18 t | 1,100 t | Estonia |
| 2010s | 203.5 t | 514.16 t | 310.66 t | New Caledonia |
| 2020s | 760.92 t | 636.2 t | 124.72 t | Estonia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland — burning crop residues, Estonia or New Caledonia?
- Estonia, at 1,150 t against 1,090 t in New Caledonia as of 2024.
- What is the difference in grassland — burning crop residues between Estonia and New Caledonia?
- 60 t, with Estonia ahead.
- How many years of comparable data are there for Estonia and New Caledonia?
- 33 years are reported by both, from 1992 to 2024.
- How do Estonia and New Caledonia rank globally for grassland — burning crop residues?
- Estonia ranks 113th and New Caledonia ranks 114th of 220 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland — 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.