Eswatini vs Solomon Islands: Drained organic soils — Emissions (CO2)
Eswatini
3.3 kt
in 2024
Solomon Islands
0.7042 kt
in 2024
Eswatini rank
100th
Solomon Islands rank
102nd
Drained organic soils — Emissions (CO2) over time
- Eswatini
- Solomon Islands
How they compare
Eswatini currently reports 3.3 kt against 0.7042 kt in Solomon Islands, a difference of 2.6 kt.
That makes Eswatini's figure about 4.7 times Solomon Islands's.
Across all 35 years both countries report, Eswatini has been ahead every year.
Eswatini ranks 100th and Solomon Islands ranks 102nd of 221 countries.
Eswatini has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Eswatini | Solomon Islands | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 2.78 kt | 0.4596 kt | 2.32 kt | Eswatini |
| 2000s | 3.16 kt | 0.4596 kt | 2.7 kt | Eswatini |
| 2010s | 3.23 kt | 0.4841 kt | 2.75 kt | Eswatini |
| 2020s | 3.3 kt | 0.7042 kt | 2.59 kt | Eswatini |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher drained organic soils — emissions, Eswatini or Solomon Islands?
- Eswatini, at 3.3 kt against 0.7042 kt in Solomon Islands as of 2024.
- What is the difference in drained organic soils — emissions between Eswatini and Solomon Islands?
- 2.6 kt, with Eswatini ahead.
- How many years of comparable data are there for Eswatini and Solomon Islands?
- 35 years are reported by both, from 1990 to 2024.
- How do Eswatini and Solomon Islands rank globally for drained organic soils — emissions?
- Eswatini ranks 100th and Solomon Islands ranks 102nd 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.