China, Hong Kong SAR vs Samoa: Forest fires — Burning crop residues
China, Hong Kong SAR
0 t
in 2024
Samoa
0 t
in 2024
China, Hong Kong SAR rank
112th
Samoa rank
112th
Forest fires — Burning crop residues over time
- China, Hong Kong SAR
- Samoa
How they compare
China, Hong Kong SAR currently reports 0 t against 0 t in Samoa, a difference of 0 t.
The two have swapped places 6 times across 35 shared years of data; in 1990 it was Samoa ahead.
China, Hong Kong SAR ranks 112th and Samoa ranks 112th of 219 countries.
Across the 4 decades both report, China, Hong Kong SAR averaged higher in 1 and Samoa in 2.
Head to head by decade
| Decade | China, Hong Kong SAR | Samoa | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 1,565 t | 7,048 t | 5,483 t | Samoa |
| 2000s | 2,852 t | 189.1 t | 2,663 t | China, Hong Kong SAR |
| 2010s | 539.57 t | 5,438 t | 4,898 t | Samoa |
| 2020s | 0 t | 0 t | 0 t | — |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher forest fires — burning crop residues, China, Hong Kong SAR or Samoa?
- China, Hong Kong SAR, at 0 t against 0 t in Samoa as of 2024.
- What is the difference in forest fires — burning crop residues between China, Hong Kong SAR and Samoa?
- 0 t, with China, Hong Kong SAR ahead.
- How many years of comparable data are there for China, Hong Kong SAR and Samoa?
- 35 years are reported by both, from 1990 to 2024.
- How do China, Hong Kong SAR and Samoa rank globally for forest fires — burning crop residues?
- China, Hong Kong SAR ranks 112th and Samoa ranks 112th of 219 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Forest fires — 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.