China, Hong Kong SAR vs Kenya: Woody savanna — Burning crop residues
China, Hong Kong SAR
0 t
in 2024
Kenya
128.22 t
in 2024
China, Hong Kong SAR rank
98th
Kenya rank
96th
Woody savanna — Burning crop residues over time
- China, Hong Kong SAR
- Kenya
How they compare
Kenya currently reports 128.22 t against 0 t in China, Hong Kong SAR, a difference of 128.22 t.
The two have swapped places 4 times across 35 shared years of data; in 1990 it was Kenya ahead.
China, Hong Kong SAR ranks 98th and Kenya ranks 96th of 220 countries.
Kenya has averaged higher in every one of the 4 decades both report.
Head to head by decade
| Decade | China, Hong Kong SAR | Kenya | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 652.13 t | 145,964 t | 145,311 t | Kenya |
| 2000s | 813.36 t | 28,525 t | 27,712 t | Kenya |
| 2010s | 371.92 t | 3,181 t | 2,809 t | Kenya |
| 2020s | 0 t | 1,383 t | 1,383 t | Kenya |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher woody savanna — burning crop residues, China, Hong Kong SAR or Kenya?
- Kenya, at 128.22 t against 0 t in China, Hong Kong SAR as of 2024.
- What is the difference in woody savanna — burning crop residues between China, Hong Kong SAR and Kenya?
- 128.22 t, with Kenya ahead.
- How many years of comparable data are there for China, Hong Kong SAR and Kenya?
- 35 years are reported by both, from 1990 to 2024.
- How do China, Hong Kong SAR and Kenya rank globally for woody savanna — burning crop residues?
- China, Hong Kong SAR ranks 98th and Kenya ranks 96th of 220 countries.
- Where does this data come from?
- Food and Agriculture Organization of the United Nations, published as Woody savanna — 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.