Niger vs Sudan: Internal renewable freshwater resources by region
Niger
3.5 billion cubic meters
in 2022
Sudan
4 billion cubic meters
in 2022
Niger rank
144th
Sudan rank
142nd
Internal renewable freshwater resources by region over time
- Niger
- Sudan
How they compare
Sudan currently reports 4 billion cubic meters against 3.5 billion cubic meters in Niger, a difference of 0.5 billion cubic meters.
That makes Sudan's figure about 1.1 times Niger's.
Across all 11 years both countries report, Sudan has been ahead every year.
Niger ranks 144th and Sudan ranks 142nd of 183 countries.
Sudan has averaged higher in every one of the 2 decades both report.
Head to head by decade
| Decade | Niger | Sudan | Difference | Ahead |
|---|---|---|---|---|
| 2010s | 3.5 billion cubic meters | 4 billion cubic meters | 0.5 billion cubic meters | Sudan |
| 2020s | 3.5 billion cubic meters | 4 billion cubic meters | 0.5 billion cubic meters | Sudan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher internal renewable freshwater resources by region, Niger or Sudan?
- Sudan, at 4 billion cubic meters against 3.5 billion cubic meters in Niger as of 2022.
- What is the difference in internal renewable freshwater resources by region between Niger and Sudan?
- 0.5 billion cubic meters, with Sudan ahead.
- How many years of comparable data are there for Niger and Sudan?
- 11 years are reported by both, from 2012 to 2022.
- How do Niger and Sudan rank globally for internal renewable freshwater resources by region?
- Niger ranks 144th and Sudan ranks 142nd of 183 countries.
- Where does this data come from?
- AQUASTAT - FAO's Global Information System on Water and Agriculture, FAO, via World Bank (2026) β processed by Our World in Data, published as Internal renewable freshwater resources by region. Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
Renewable internal freshwater resources refers to the quantity of internal freshwater from inflowing river basins and recharging groundwater aquifers.