Hungary vs Papua New Guinea: Cropland organic soils — Emissions (N2O)
Hungary
3.66 kt
in 2024
Papua New Guinea
3.84 kt
in 2024
Hungary rank
15th
Papua New Guinea rank
14th
Cropland organic soils — Emissions (N2O) over time
- Hungary
- Papua New Guinea
How they compare
Papua New Guinea currently reports 3.84 kt against 3.66 kt in Hungary, a difference of 0.18 kt.
The two have swapped places 1 time across 35 shared years of data; in 1990 it was Hungary ahead.
Hungary ranks 15th and Papua New Guinea ranks 14th of 242 countries.
Across the 4 decades both report, Hungary averaged higher in 1 and Papua New Guinea in 3.
Head to head by decade
| Decade | Hungary | Papua New Guinea | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 3.75 kt | 3.33 kt | 0.4187 kt | Hungary |
| 2000s | 3.7 kt | 3.9 kt | 0.196 kt | Papua New Guinea |
| 2010s | 3.68 kt | 3.73 kt | 0.0474 kt | Papua New Guinea |
| 2020s | 3.66 kt | 3.83 kt | 0.1676 kt | Papua New Guinea |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Hungary or Papua New Guinea?
- Papua New Guinea, at 3.84 kt against 3.66 kt in Hungary as of 2024.
- What is the difference in cropland organic soils — emissions between Hungary and Papua New Guinea?
- 0.18 kt, with Papua New Guinea ahead.
- How many years of comparable data are there for Hungary and Papua New Guinea?
- 35 years are reported by both, from 1990 to 2024.
- How do Hungary and Papua New Guinea rank globally for cropland organic soils — emissions?
- Hungary ranks 15th and Papua New Guinea ranks 14th of 242 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland organic soils — 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 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.