Mongolia vs Papua New Guinea: Drained organic soils — Emissions (CO2)
Mongolia
22,193 kt
in 2024
Papua New Guinea
22,096 kt
in 2024
Mongolia rank
10th
Papua New Guinea rank
11th
Drained organic soils — Emissions (CO2) over time
- Mongolia
- Papua New Guinea
How they compare
Mongolia currently reports 22,193 kt against 22,096 kt in Papua New Guinea, a difference of 97 kt.
The two have swapped places 2 times across 35 shared years of data; in 1990 it was Mongolia ahead.
Mongolia ranks 10th and Papua New Guinea ranks 11th of 221 countries.
Mongolia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Mongolia | Papua New Guinea | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 22,234 kt | 18,780 kt | 3,454 kt | Mongolia |
| 2000s | 22,390 kt | 22,341 kt | 49.25 kt | Mongolia |
| 2010s | 22,456 kt | 21,298 kt | 1,158 kt | Mongolia |
| 2020s | 22,212 kt | 21,988 kt | 224.1 kt | Mongolia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Mongolia or Papua New Guinea?
- Mongolia, at 22,193 kt against 22,096 kt in Papua New Guinea as of 2024.
- What is the difference in drained organic soils — emissions between Mongolia and Papua New Guinea?
- 97 kt, with Mongolia ahead.
- How many years of comparable data are there for Mongolia and Papua New Guinea?
- 35 years are reported by both, from 1990 to 2024.
- How do Mongolia and Papua New Guinea rank globally for drained organic soils — emissions?
- Mongolia ranks 10th and Papua New Guinea ranks 11th of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Drained organic soils — Emissions (CO2). 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 drained organic soils consists of nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from the mineralization and oxidation of organic matter in organic soils that are drained for agricultural activities.