Central Asia vs Myanmar: Savanna — Burning crop residues
Central Asia
5,735 t
in 2024
Myanmar
1.92 million t
in 2024
Central Asia rank
29th
Myanmar rank
27th
Savanna — Burning crop residues over time
- Central Asia
- Myanmar
How they compare
Myanmar currently reports 1.92 million t against 5,735 t in Central Asia, a difference of 1.91 million t.
That makes Myanmar's figure about 334.3 times Central Asia's.
Across all 33 years both countries report, Myanmar has been ahead every year.
Central Asia ranks 29th and Myanmar ranks 27th of 31 groups.
Myanmar has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Central Asia | Myanmar | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 49,941 t | 941,115 t | 891,174 t | Myanmar |
| 2000s | 70,151 t | 1.71 million t | 1.64 million t | Myanmar |
| 2010s | 25,372 t | 2.04 million t | 2.02 million t | Myanmar |
| 2020s | 62,082 t | 1.67 million t | 1.61 million t | Myanmar |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher savanna — burning crop residues, Central Asia or Myanmar?
- Myanmar, at 1.92 million t against 5,735 t in Central Asia as of 2024.
- What is the difference in savanna — burning crop residues between Central Asia and Myanmar?
- 1.91 million t, with Myanmar ahead.
- How many years of comparable data are there for Central Asia and Myanmar?
- 33 years are reported by both, from 1992 to 2024.
- How do Central Asia and Myanmar rank globally for savanna — burning crop residues?
- Central Asia ranks 29th and Myanmar ranks 27th of 31 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Savanna — 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.