Ecuador vs Thailand: Closed and open shrubland — Burning crop residues
Ecuador
570.6 t
in 2024
Thailand
305.9 t
in 2024
Ecuador rank
52nd
Thailand rank
54th
Closed and open shrubland — Burning crop residues over time
- Ecuador
- Thailand
How they compare
Ecuador currently reports 570.6 t against 305.9 t in Thailand, a difference of 264.7 t.
That makes Ecuador's figure about 1.9 times Thailand's.
The two have swapped places 7 times across 35 shared years of data; in 1990 it was Thailand ahead.
Ecuador ranks 52nd and Thailand ranks 54th of 219 countries.
Thailand has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Ecuador | Thailand | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 4,501 t | 45,663 t | 41,161 t | Thailand |
| 2000s | 2,186 t | 8,112 t | 5,926 t | Thailand |
| 2010s | 171.17 t | 3,255 t | 3,084 t | Thailand |
| 2020s | 114.12 t | 595.62 t | 481.5 t | Thailand |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Ecuador or Thailand?
- Ecuador, at 570.6 t against 305.9 t in Thailand as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Ecuador and Thailand?
- 264.7 t, with Ecuador ahead.
- How many years of comparable data are there for Ecuador and Thailand?
- 35 years are reported by both, from 1990 to 2024.
- How do Ecuador and Thailand rank globally for closed and open shrubland — burning crop residues?
- Ecuador ranks 52nd and Thailand ranks 54th 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.