Iran (Islamic Republic of) vs Mexico: Closed shrubland — Emissions (N2O)
Iran (Islamic Republic of)
0 kt
in 2024
Mexico
0.0262 kt
in 2024
Iran (Islamic Republic of) rank
8th
Mexico rank
10th
Closed shrubland — Emissions (N2O) over time
- Iran (Islamic Republic of)
- Mexico
How they compare
Mexico currently reports 0.0262 kt against 0 kt in Iran (Islamic Republic of), a difference of 0.0262 kt.
Across all 35 years both countries report, Mexico has been ahead every year.
Iran (Islamic Republic of) ranks 8th and Mexico ranks 10th of 21 countries.
Mexico has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | Iran (Islamic Republic of) | Mexico | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 0.007 kt | 0.2006 kt | 0.1936 kt | Mexico |
| 2000s | 0.0016 kt | 0.1125 kt | 0.1109 kt | Mexico |
| 2010s | 0 kt | 0.0675 kt | 0.0675 kt | Mexico |
| 2020s | 0 kt | 0.077 kt | 0.077 kt | Mexico |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher closed shrubland — emissions, Iran (Islamic Republic of) or Mexico?
- Mexico, at 0.0262 kt against 0 kt in Iran (Islamic Republic of) as of 2024.
- What is the difference in closed shrubland — emissions between Iran (Islamic Republic of) and Mexico?
- 0.0262 kt, with Mexico ahead.
- How many years of comparable data are there for Iran (Islamic Republic of) and Mexico?
- 35 years are reported by both, from 1990 to 2024.
- How do Iran (Islamic Republic of) and Mexico rank globally for closed shrubland — emissions?
- Iran (Islamic Republic of) ranks 8th and Mexico ranks 10th of 21 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Closed shrubland — Emissions (N2O). 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.