Angola vs Liechtenstein: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Angola
- Liechtenstein
How they compare
Liechtenstein currently reports 0.1898 against 0.1666 in Angola, a difference of 0.0232.
That makes Liechtenstein's figure about 1.1 times Angola's.
The two have swapped places 29 times across 64 shared years of data; in 1960 it was Angola ahead.
Angola ranks 60th and Liechtenstein ranks 57th of 188 countries.
Across the 7 decades both report, Angola averaged higher in 4 and Liechtenstein in 3.
Head to head by decade
| Decade | Angola | Liechtenstein | Difference | Ahead |
|---|---|---|---|---|
| 1960s | 1.04 | 0.2962 | 0.7457 | Angola |
| 1970s | 0.2626 | 0.3257 | 0.0631 | Liechtenstein |
| 1980s | -0.8575 | 0.4171 | 1.27 | Liechtenstein |
| 1990s | -0.494 | 0.0602 | 0.5542 | Liechtenstein |
| 2000s | 0.1251 | -0.3035 | 0.4286 | Angola |
| 2010s | -0.0007 | -0.3736 | 0.373 | Angola |
| 2020s | 0.1831 | -0.4413 | 0.6244 | Angola |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Angola or Liechtenstein?
- Liechtenstein, at 0.1898 against 0.1666 in Angola as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Angola and Liechtenstein?
- 0.0232, with Liechtenstein ahead.
- How many years of comparable data are there for Angola and Liechtenstein?
- 64 years are reported by both, from 1960 to 2023.
- How do Angola and Liechtenstein rank globally for standardised precipitation-evapotranspiration index?
- Angola ranks 60th and Liechtenstein ranks 57th 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.