Bangladesh vs Madagascar: Grassland organic soils — Emissions
Bangladesh
1,046 kt
in 2024
Madagascar
917.14 kt
in 2024
Bangladesh rank
30th
Madagascar rank
33rd
Grassland organic soils — Emissions over time
- Bangladesh
- Madagascar
How they compare
Bangladesh currently reports 1,046 kt against 917.14 kt in Madagascar, a difference of 128.86 kt.
That makes Bangladesh's figure about 1.1 times Madagascar's.
Across all 35 years both countries report, Bangladesh has been ahead every year.
Bangladesh ranks 30th and Madagascar ranks 33rd of 221 countries.
Bangladesh has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Bangladesh | Madagascar | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1,048 kt | 928.04 kt | 120.07 kt | Bangladesh |
| 2000s | 1,033 kt | 934.27 kt | 98.27 kt | Bangladesh |
| 2010s | 1,036 kt | 920.78 kt | 115.23 kt | Bangladesh |
| 2020s | 1,033 kt | 919.67 kt | 113.48 kt | Bangladesh |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher grassland organic soils — emissions, Bangladesh or Madagascar?
- Bangladesh, at 1,046 kt against 917.14 kt in Madagascar as of 2024.
- What is the difference in grassland organic soils — emissions between Bangladesh and Madagascar?
- 128.86 kt, with Bangladesh ahead.
- How many years of comparable data are there for Bangladesh and Madagascar?
- 35 years are reported by both, from 1990 to 2024.
- How do Bangladesh and Madagascar rank globally for grassland organic soils — emissions?
- Bangladesh ranks 30th and Madagascar ranks 33rd 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.