Central Asia vs Peru: Open shrubland — Burning crop residues
Central Asia
37,161 t
in 2024
Peru
31,202 t
in 2024
Central Asia rank
22nd
Peru rank
23rd
Open shrubland — Burning crop residues over time
- Central Asia
- Peru
How they compare
Central Asia currently reports 37,161 t against 31,202 t in Peru, a difference of 5,959 t.
That makes Central Asia's figure about 1.2 times Peru's.
The two have swapped places 4 times across 33 shared years of data; in 1992 it was Central Asia ahead.
Central Asia ranks 22nd and Peru ranks 23rd of 31 groups.
Central Asia has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Central Asia | Peru | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1.40 million t | 34,633 t | 1.37 million t | Central Asia |
| 2000s | 232,642 t | 2,750 t | 229,893 t | Central Asia |
| 2010s | 120,733 t | 9,268 t | 111,465 t | Central Asia |
| 2020s | 118,919 t | 18,598 t | 100,321 t | Central Asia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher open shrubland — burning crop residues, Central Asia or Peru?
- Central Asia, at 37,161 t against 31,202 t in Peru as of 2024.
- What is the difference in open shrubland — burning crop residues between Central Asia and Peru?
- 5,959 t, with Central Asia ahead.
- How many years of comparable data are there for Central Asia and Peru?
- 33 years are reported by both, from 1992 to 2024.
- How do Central Asia and Peru rank globally for open shrubland — burning crop residues?
- Central Asia ranks 22nd and Peru ranks 23rd of 31 groups.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as 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.