Myanmar vs Nicaragua: Closed shrubland — Burning crop residues
Myanmar
16,578 t
in 2024
Nicaragua
63,384 t
in 2023
Myanmar rank
16th
Nicaragua rank
15th
Closed shrubland — Burning crop residues over time
- Myanmar
- Nicaragua
How they compare
Nicaragua currently reports 63,384 t against 16,578 t in Myanmar, a difference of 46,806 t.
That makes Nicaragua's figure about 3.8 times Myanmar's.
The two have swapped places 5 times across 34 shared years of data; in 1990 it was Myanmar ahead.
Myanmar ranks 16th and Nicaragua ranks 15th of 219 countries.
Across the 4 decades both report, Myanmar averaged higher in 1 and Nicaragua in 3.
Head to head by decade
| Decade | Myanmar | Nicaragua | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 45,108 t | 19,564 t | 25,544 t | Myanmar |
| 2000s | 17,525 t | 25,342 t | 7,816 t | Nicaragua |
| 2010s | 2,058 t | 12,963 t | 10,905 t | Nicaragua |
| 2020s | 6,574 t | 18,987 t | 12,413 t | Nicaragua |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Myanmar or Nicaragua?
- Nicaragua, at 63,384 t against 16,578 t in Myanmar as of 2023.
- What is the difference in closed shrubland — burning crop residues between Myanmar and Nicaragua?
- 46,806 t, with Nicaragua ahead.
- How many years of comparable data are there for Myanmar and Nicaragua?
- 34 years are reported by both, from 1990 to 2023.
- How do Myanmar and Nicaragua rank globally for closed shrubland — burning crop residues?
- Myanmar ranks 16th and Nicaragua ranks 15th 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.