Cameroon vs Jordan: Closed and open shrubland — Burning crop residues
Cameroon
1,712 t
in 2024
Jordan
920.31 t
in 2024
Cameroon rank
45th
Jordan rank
48th
Closed and open shrubland — Burning crop residues over time
- Cameroon
- Jordan
How they compare
Cameroon currently reports 1,712 t against 920.31 t in Jordan, a difference of 791.69 t.
That makes Cameroon's figure about 1.9 times Jordan's.
The two have swapped places 12 times across 35 shared years of data; in 1990 it was Cameroon ahead.
Cameroon ranks 45th and Jordan ranks 48th of 219 countries.
Cameroon has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Cameroon | Jordan | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 758,591 t | 429.78 t | 758,161 t | Cameroon |
| 2000s | 135,710 t | 70.71 t | 135,640 t | Cameroon |
| 2010s | 970.05 t | 30.67 t | 939.38 t | Cameroon |
| 2020s | 2,168 t | 368.12 t | 1,800 t | Cameroon |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed and open shrubland — burning crop residues, Cameroon or Jordan?
- Cameroon, at 1,712 t against 920.31 t in Jordan as of 2024.
- What is the difference in closed and open shrubland — burning crop residues between Cameroon and Jordan?
- 791.69 t, with Cameroon ahead.
- How many years of comparable data are there for Cameroon and Jordan?
- 35 years are reported by both, from 1990 to 2024.
- How do Cameroon and Jordan rank globally for closed and open shrubland — burning crop residues?
- Cameroon ranks 45th and Jordan ranks 48th 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.