Colombia vs Eastern Asia: Closed shrubland — Emissions (CH4)
Colombia
0.0197 kt
in 2024
Eastern Asia
0.004 kt
in 2024
Colombia rank
19th
Eastern Asia rank
18th
Closed shrubland — Emissions (CH4) over time
- Colombia
- Eastern Asia
How they compare
Colombia currently reports 0.0197 kt against 0.004 kt in Eastern Asia, a difference of 0.0157 kt.
That makes Colombia's figure about 4.9 times Eastern Asia's.
The two have swapped places 9 times across 35 shared years of data; in 1990 it was Eastern Asia ahead.
Colombia ranks 19th and Eastern Asia ranks 18th of 219 countries.
Across the 4 decades both report, Colombia averaged higher in 2 and Eastern Asia in 2.
Head to head by decade
| Decade | Colombia | Eastern Asia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.1509 kt | 0.4943 kt | 0.3433 kt | Eastern Asia |
| 2000s | 0.1011 kt | 0.1289 kt | 0.0278 kt | Eastern Asia |
| 2010s | 0.0389 kt | 0.0275 kt | 0.0113 kt | Colombia |
| 2020s | 0.0121 kt | 0.0032 kt | 0.0089 kt | Colombia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — emissions, Colombia or Eastern Asia?
- Colombia, at 0.0197 kt against 0.004 kt in Eastern Asia as of 2024.
- What is the difference in closed shrubland — emissions between Colombia and Eastern Asia?
- 0.0157 kt, with Colombia ahead.
- How many years of comparable data are there for Colombia and Eastern Asia?
- 35 years are reported by both, from 1990 to 2024.
- How do Colombia and Eastern Asia rank globally for closed shrubland — emissions?
- Colombia ranks 19th and Eastern Asia ranks 18th 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.