Argentina vs Niger: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Argentina
- Niger
How they compare
Niger currently reports -0.8767 against -0.8851 in Argentina, a difference of 0.0084.
The two have swapped places 24 times across 64 shared years of data; in 1960 it was Niger ahead.
Argentina ranks 130th and Niger ranks 129th of 188 countries.
Across the 7 decades both report, Argentina averaged higher in 4 and Niger in 3.
Head to head by decade
| Decade | Argentina | Niger | Difference | Ahead |
|---|---|---|---|---|
| 1960s | -0.2359 | 0.5218 | 0.7576 | Niger |
| 1970s | 0.5091 | 0.8843 | 0.3751 | Niger |
| 1980s | 0.6062 | 0.375 | 0.2311 | Argentina |
| 1990s | 0.7279 | -0.2615 | 0.9894 | Argentina |
| 2000s | 0.2056 | -0.8427 | 1.05 | Argentina |
| 2010s | -0.0043 | -0.5595 | 0.5552 | Argentina |
| 2020s | -1.53 | -0.2729 | 1.26 | Niger |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Argentina or Niger?
- Niger, at -0.8767 against -0.8851 in Argentina as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Argentina and Niger?
- 0.0084, with Niger ahead.
- How many years of comparable data are there for Argentina and Niger?
- 64 years are reported by both, from 1960 to 2023.
- How do Argentina and Niger rank globally for standardised precipitation-evapotranspiration index?
- Argentina ranks 130th and Niger ranks 129th of 188 countries.
- Where does this data come from?
- Global SPEI database (SPEIbase). https://spei.csic.es/database.html, published as Standardised Precipitation-Evapotranspiration Index. Statizoid refreshes it automatically from the source and publishes the full history for both places.
Individual pages
About this data
The SPEI fulfills the requirements of a drought index since its multi-scalar character enables it to be used by different scientific disciplines to detect, monitor, and analyze droughts. Like the sc-PDSI and the SPI, the SPEI can measure drought severity according to its intensity and duration, and can identify the onset and end of drought episodes. The SPEI allows comparison of drought severity through time and space, since it can be calculated over a wide range of climates, as can the SPI.