Azerbaijan vs New Zealand: Savanna — Burning crop residues
Azerbaijan
1,674 t
in 2024
New Zealand
1,499 t
in 2024
Azerbaijan rank
93rd
New Zealand rank
96th
Savanna — Burning crop residues over time
- Azerbaijan
- New Zealand
How they compare
Azerbaijan currently reports 1,674 t against 1,499 t in New Zealand, a difference of 175 t.
That makes Azerbaijan's figure about 1.1 times New Zealand's.
The two have swapped places 10 times across 33 shared years of data; in 1992 it was Azerbaijan ahead.
Azerbaijan ranks 93rd and New Zealand ranks 96th of 221 countries.
Azerbaijan has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Azerbaijan | New Zealand | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 6,672 t | 411.29 t | 6,261 t | Azerbaijan |
| 2000s | 1,238 t | 431.89 t | 805.74 t | Azerbaijan |
| 2010s | 3,445 t | 1,614 t | 1,831 t | Azerbaijan |
| 2020s | 2,573 t | 634.54 t | 1,938 t | Azerbaijan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, Azerbaijan or New Zealand?
- Azerbaijan, at 1,674 t against 1,499 t in New Zealand as of 2024.
- What is the difference in savanna — burning crop residues between Azerbaijan and New Zealand?
- 175 t, with Azerbaijan ahead.
- How many years of comparable data are there for Azerbaijan and New Zealand?
- 33 years are reported by both, from 1992 to 2024.
- How do Azerbaijan and New Zealand rank globally for savanna — burning crop residues?
- Azerbaijan ranks 93rd and New Zealand ranks 96th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as 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.