Ethiopia vs Zambia: Closed and open shrubland — Burning crop residues
Ethiopia
174,030 t
in 2024
Zambia
176,405 t
in 2024
Ethiopia rank
19th
Zambia rank
18th
Closed and open shrubland — Burning crop residues over time
- Ethiopia
- Zambia
How they compare
Zambia currently reports 176,405 t against 174,030 t in Ethiopia, a difference of 2,375 t.
The two have swapped places 6 times across 32 shared years of data; in 1993 it was Zambia ahead.
Ethiopia ranks 19th and Zambia ranks 18th of 219 countries.
Across the 4 decades both report, Ethiopia averaged higher in 1 and Zambia in 3.
Head to head by decade
| Decade | Ethiopia | Zambia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.06 million t | 3.27 million t | 2.21 million t | Zambia |
| 2000s | 270,499 t | 892,242 t | 621,744 t | Zambia |
| 2010s | 95,618 t | 457,844 t | 362,227 t | Zambia |
| 2020s | 220,584 t | 151,809 t | 68,775 t | Ethiopia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Ethiopia or Zambia?
- Zambia, at 176,405 t against 174,030 t in Ethiopia as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Ethiopia and Zambia?
- 2,375 t, with Zambia ahead.
- How many years of comparable data are there for Ethiopia and Zambia?
- 32 years are reported by both, from 1993 to 2024.
- How do Ethiopia and Zambia rank globally for closed and open shrubland — burning crop residues?
- Ethiopia ranks 19th and Zambia ranks 18th 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.