Croatia vs Faroe Islands: Cropland organic soils — Emissions (CO2)
Croatia
9.19 kt
in 2024
Faroe Islands
11.46 kt
in 2024
Croatia rank
101st
Faroe Islands rank
100th
Cropland organic soils — Emissions (CO2) over time
- Croatia
- Faroe Islands
How they compare
Faroe Islands currently reports 11.46 kt against 9.19 kt in Croatia, a difference of 2.27 kt.
That makes Faroe Islands's figure about 1.2 times Croatia's.
Across all 33 years both countries report, Faroe Islands has been ahead every year.
Croatia ranks 101st and Faroe Islands ranks 100th of 242 countries.
Faroe Islands has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Croatia | Faroe Islands | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 7.24 kt | 9.89 kt | 2.65 kt | Faroe Islands |
| 2000s | 8.49 kt | 9.89 kt | 1.4 kt | Faroe Islands |
| 2010s | 9.65 kt | 9.94 kt | 0.2904 kt | Faroe Islands |
| 2020s | 9.19 kt | 11.46 kt | 2.28 kt | Faroe Islands |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher cropland organic soils — emissions, Croatia or Faroe Islands?
- Faroe Islands, at 11.46 kt against 9.19 kt in Croatia as of 2024.
- What is the difference in cropland organic soils — emissions between Croatia and Faroe Islands?
- 2.27 kt, with Faroe Islands ahead.
- How many years of comparable data are there for Croatia and Faroe Islands?
- 33 years are reported by both, from 1992 to 2024.
- How do Croatia and Faroe Islands rank globally for cropland organic soils — emissions?
- Croatia ranks 101st and Faroe Islands ranks 100th of 242 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Cropland 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.