Colombia vs Southern Asia: Closed shrubland — Emissions
Colombia
0.0197 kt
in 2024
Southern Asia
0.0013 kt
in 2024
Colombia rank
19th
Southern Asia rank
19th
Closed shrubland — Emissions over time
- Colombia
- Southern Asia
How they compare
Colombia currently reports 0.0197 kt against 0.0013 kt in Southern Asia, a difference of 0.0184 kt.
That makes Colombia's figure about 15.2 times Southern Asia's.
The two have swapped places 1 time across 35 shared years of data; in 1990 it was Southern Asia ahead.
Colombia ranks 19th and Southern Asia ranks 19th of 219 countries.
Across the 4 decades both report, Colombia averaged higher in 3 and Southern Asia in 1.
Head to head by decade
| Decade | Colombia | Southern Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.1509 kt | 0.3211 kt | 0.1701 kt | Southern Asia |
| 2000s | 0.1011 kt | 0.0518 kt | 0.0493 kt | Colombia |
| 2010s | 0.0389 kt | 0.0001 kt | 0.0387 kt | Colombia |
| 2020s | 0.0121 kt | 0.0005 kt | 0.0115 kt | Colombia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — emissions, Colombia or Southern Asia?
- Colombia, at 0.0197 kt against 0.0013 kt in Southern Asia as of 2024.
- What is the difference in closed shrubland — emissions between Colombia and Southern Asia?
- 0.0184 kt, with Colombia ahead.
- How many years of comparable data are there for Colombia and Southern Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Colombia and Southern Asia rank globally for closed shrubland — emissions?
- Colombia ranks 19th and Southern Asia ranks 19th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — Emissions (CH4). 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.