El Salvador vs Malaysia: Agricultural water withdrawal, Percent of total water withdrawal
El Salvador
46.27
in 2021
Malaysia
45.65
in 2021
El Salvador rank
108th
Malaysia rank
110th
Agricultural water withdrawal, Percent of total water withdrawal over time
- El Salvador
- Malaysia
How they compare
El Salvador currently reports 46.27 against 45.65 in Malaysia, a difference of 0.62.
The two have swapped places 2 times across 24 shared years of data; in 1998 it was El Salvador ahead.
El Salvador ranks 108th and Malaysia ranks 110th of 180 countries.
Across the 4 decades both report, El Salvador averaged higher in 3 and Malaysia in 1.
Head to head by decade
| Decade | El Salvador | Malaysia | Difference | Ahead |
|---|---|---|---|---|
| 1990s | 54.23 | 45.65 | 8.58 | El Salvador |
| 2000s | 63.46 | 45.65 | 17.82 | El Salvador |
| 2010s | 54.53 | 45.65 | 8.89 | El Salvador |
| 2020s | 41.84 | 45.65 | 3.81 | Malaysia |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher agricultural water withdrawal, percent of total water withdrawal, El Salvador or Malaysia?
- El Salvador, at 46.27 against 45.65 in Malaysia as of 2021.
- What is the difference in agricultural water withdrawal, percent of total water withdrawal between El Salvador and Malaysia?
- 0.62, with El Salvador ahead.
- How many years of comparable data are there for El Salvador and Malaysia?
- 24 years are reported by both, from 1998 to 2021.
- How do El Salvador and Malaysia rank globally for agricultural water withdrawal, percent of total water withdrawal?
- El Salvador ranks 108th and Malaysia ranks 110th of 180 countries.
- Where does this data come from?
- International Monetary Fund, published as Agricultural water withdrawal, Percent of total water withdrawal (Not Applicable). Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
This dataset provides information on global climate and weather patterns, providing insights into temperature variations, land cover accounts, and shifts in mean sea levels.