Myanmar vs Somalia: Closed and open shrubland — Burning crop residues
Myanmar
16,578 t
in 2024
Somalia
13,447 t
in 2024
Myanmar rank
30th
Somalia rank
32nd
Closed and open shrubland — Burning crop residues over time
- Myanmar
- Somalia
How they compare
Myanmar currently reports 16,578 t against 13,447 t in Somalia, a difference of 3,131 t.
That makes Myanmar's figure about 1.2 times Somalia's.
The two have swapped places 12 times across 35 shared years of data; in 1990 it was Myanmar ahead.
Myanmar ranks 30th and Somalia ranks 32nd of 219 countries.
Across the 4 decades both report, Myanmar averaged higher in 2 and Somalia in 2.
Head to head by decade
| Decade | Myanmar | Somalia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 73,549 t | 53,345 t | 20,204 t | Myanmar |
| 2000s | 19,339 t | 10,169 t | 9,170 t | Myanmar |
| 2010s | 2,058 t | 23,112 t | 21,054 t | Somalia |
| 2020s | 8,575 t | 11,491 t | 2,917 t | Somalia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Myanmar or Somalia?
- Myanmar, at 16,578 t against 13,447 t in Somalia as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Myanmar and Somalia?
- 3,131 t, with Myanmar ahead.
- How many years of comparable data are there for Myanmar and Somalia?
- 35 years are reported by both, from 1990 to 2024.
- How do Myanmar and Somalia rank globally for closed and open shrubland — burning crop residues?
- Myanmar ranks 30th and Somalia ranks 32nd of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed and open 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.