Madagascar vs Myanmar: Closed shrubland — Burning crop residues
Madagascar
97,744 t
in 2024
Myanmar
16,578 t
in 2024
Madagascar rank
13th
Myanmar rank
16th
Closed shrubland — Burning crop residues over time
- Madagascar
- Myanmar
How they compare
Madagascar currently reports 97,744 t against 16,578 t in Myanmar, a difference of 81,166 t.
That makes Madagascar's figure about 5.9 times Myanmar's.
Across all 35 years both countries report, Madagascar has been ahead every year.
Madagascar ranks 13th and Myanmar ranks 16th of 219 countries.
Madagascar has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Madagascar | Myanmar | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 861,191 t | 45,108 t | 816,083 t | Madagascar |
| 2000s | 1.42 million t | 17,525 t | 1.40 million t | Madagascar |
| 2010s | 710,989 t | 2,058 t | 708,931 t | Madagascar |
| 2020s | 273,907 t | 8,575 t | 265,332 t | Madagascar |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Madagascar or Myanmar?
- Madagascar, at 97,744 t against 16,578 t in Myanmar as of 2024.
- What is the difference in closed shrubland — burning crop residues between Madagascar and Myanmar?
- 81,166 t, with Madagascar ahead.
- How many years of comparable data are there for Madagascar and Myanmar?
- 35 years are reported by both, from 1990 to 2024.
- How do Madagascar and Myanmar rank globally for closed shrubland — burning crop residues?
- Madagascar ranks 13th and Myanmar ranks 16th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — Burning crop residues (Biomass burned, dry matter). 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 Fires consists of estimates of methane (CH4), nitrous oxide (N2O) and carbon dioxide (CO2) emissions generated from biomass burning in a range of vegetation types and from fires in organic soils.