Malaysia vs Southern Africa: Grassland organic soils — Emissions
Malaysia
1,704 kt
in 2024
Southern Africa
370.08 kt
in 2024
Malaysia rank
21st
Southern Africa rank
23rd
Grassland organic soils — Emissions over time
- Malaysia
- Southern Africa
How they compare
Malaysia currently reports 1,704 kt against 370.08 kt in Southern Africa, a difference of 1,334 kt.
That makes Malaysia's figure about 4.6 times Southern Africa's.
Across all 35 years both countries report, Malaysia has been ahead every year.
Malaysia ranks 21st and Southern Africa ranks 23rd of 221 countries.
Malaysia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Malaysia | Southern Africa | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1,552 kt | 305.9 kt | 1,246 kt | Malaysia |
| 2000s | 1,606 kt | 364.35 kt | 1,241 kt | Malaysia |
| 2010s | 1,724 kt | 371.98 kt | 1,352 kt | Malaysia |
| 2020s | 1,715 kt | 370.06 kt | 1,345 kt | Malaysia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — emissions, Malaysia or Southern Africa?
- Malaysia, at 1,704 kt against 370.08 kt in Southern Africa as of 2024.
- What is the difference in grassland organic soils — emissions between Malaysia and Southern Africa?
- 1,334 kt, with Malaysia ahead.
- How many years of comparable data are there for Malaysia and Southern Africa?
- 35 years are reported by both, from 1990 to 2024.
- How do Malaysia and Southern Africa rank globally for grassland organic soils — emissions?
- Malaysia ranks 21st and Southern Africa ranks 23rd of 221 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Grassland 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.