Guatemala vs Southern Asia: Woody savanna — Emissions
Guatemala
0.1171 kt
in 2024
Southern Asia
0.3091 kt
in 2024
Guatemala rank
20th
Southern Asia rank
18th
Woody savanna — Emissions over time
- Guatemala
- Southern Asia
How they compare
Southern Asia currently reports 0.3091 kt against 0.1171 kt in Guatemala, a difference of 0.192 kt.
That makes Southern Asia's figure about 2.6 times Guatemala's.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was Southern Asia ahead.
Guatemala ranks 20th and Southern Asia ranks 18th of 220 countries.
Southern Asia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Guatemala | Southern Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.0856 kt | 0.2975 kt | 0.2119 kt | Southern Asia |
| 2000s | 0.1733 kt | 0.2932 kt | 0.1199 kt | Southern Asia |
| 2010s | 0.0966 kt | 0.287 kt | 0.1904 kt | Southern Asia |
| 2020s | 0.0663 kt | 0.2444 kt | 0.1781 kt | Southern Asia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher woody savanna — emissions, Guatemala or Southern Asia?
- Southern Asia, at 0.3091 kt against 0.1171 kt in Guatemala as of 2024.
- What is the difference in woody savanna — emissions between Guatemala and Southern Asia?
- 0.192 kt, with Southern Asia ahead.
- How many years of comparable data are there for Guatemala and Southern Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Guatemala and Southern Asia rank globally for woody savanna — emissions?
- Guatemala ranks 20th and Southern Asia ranks 18th of 220 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Woody savanna — Emissions (N2O). 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.