Kenya vs Southern Europe: Closed shrubland — Burning crop residues
Kenya
5,135 t
in 2024
Southern Europe
0 t
in 2024
Kenya rank
20th
Southern Europe rank
20th
Closed shrubland — Burning crop residues over time
- Kenya
- Southern Europe
How they compare
Kenya currently reports 5,135 t against 0 t in Southern Europe, a difference of 5,135 t.
The two have swapped places 15 times across 35 shared years of data; in 1990 it was Southern Europe ahead.
Kenya ranks 20th and Southern Europe ranks 20th of 219 countries.
Across the 4 decades both report, Kenya averaged higher in 1 and Southern Europe in 3.
Head to head by decade
| Decade | Kenya | Southern Europe | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 284,077 t | 272,972 t | 11,105 t | Kenya |
| 2000s | 54,037 t | 118,262 t | 64,224 t | Southern Europe |
| 2010s | 32,580 t | 32,987 t | 407.08 t | Southern Europe |
| 2020s | 16,433 t | 23,644 t | 7,211 t | Southern Europe |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — burning crop residues, Kenya or Southern Europe?
- Kenya, at 5,135 t against 0 t in Southern Europe as of 2024.
- What is the difference in closed shrubland — burning crop residues between Kenya and Southern Europe?
- 5,135 t, with Kenya ahead.
- How many years of comparable data are there for Kenya and Southern Europe?
- 35 years are reported by both, from 1990 to 2024.
- How do Kenya and Southern Europe rank globally for closed shrubland — burning crop residues?
- Kenya ranks 20th and Southern Europe ranks 20th 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.