El Salvador vs New Zealand: Savanna fires — Burned Area
El Salvador
898.21 ha
in 2024
New Zealand
795.23 ha
in 2024
El Salvador rank
113th
New Zealand rank
114th
Savanna fires — Burned Area over time
- El Salvador
- New Zealand
How they compare
El Salvador currently reports 898.21 ha against 795.23 ha in New Zealand, a difference of 102.98 ha.
That makes El Salvador's figure about 1.1 times New Zealand's.
The two have swapped places 8 times across 35 shared years of data; in 1990 it was El Salvador ahead.
El Salvador ranks 113th and New Zealand ranks 114th of 221 countries.
El Salvador has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | El Salvador | New Zealand | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 2,772 ha | 643.02 ha | 2,129 ha | El Salvador |
| 2000s | 2,394 ha | 697.46 ha | 1,696 ha | El Salvador |
| 2010s | 6,206 ha | 1,334 ha | 4,872 ha | El Salvador |
| 2020s | 2,143 ha | 1,716 ha | 427.24 ha | El Salvador |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna fires — burned area, El Salvador or New Zealand?
- El Salvador, at 898.21 ha against 795.23 ha in New Zealand as of 2024.
- What is the difference in savanna fires — burned area between El Salvador and New Zealand?
- 102.98 ha, with El Salvador ahead.
- How many years of comparable data are there for El Salvador and New Zealand?
- 35 years are reported by both, from 1990 to 2024.
- How do El Salvador and New Zealand rank globally for savanna fires — burned area?
- El Salvador ranks 113th and New Zealand ranks 114th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Savanna fires — Burned Area. 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.