Armenia vs Mozambique: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Armenia
- Mozambique
How they compare
Armenia currently reports 0.0672 against 0.0591 in Mozambique, a difference of 0.0081.
That makes Armenia's figure about 1.1 times Mozambique's.
The two have swapped places 26 times across 64 shared years of data; in 1960 it was Armenia ahead.
Armenia ranks 68th and Mozambique ranks 69th of 189 countries.
Across the 7 decades both report, Armenia averaged higher in 4 and Mozambique in 3.
Head to head by decade
| Decade | Armenia | Mozambique | Difference | Ahead |
|---|---|---|---|---|
| 1960s | 0.0282 | 0.3427 | 0.3145 | Mozambique |
| 1970s | -0.1809 | 0.2908 | 0.4717 | Mozambique |
| 1980s | 0.0328 | -0.0266 | 0.0594 | Armenia |
| 1990s | -0.236 | -0.5762 | 0.3402 | Armenia |
| 2000s | 0.2555 | -0.3227 | 0.5783 | Armenia |
| 2010s | -0.1622 | -0.2982 | 0.136 | Armenia |
| 2020s | -0.8453 | -0.3088 | 0.5365 | Mozambique |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Armenia or Mozambique?
- Armenia, at 0.0672 against 0.0591 in Mozambique as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Armenia and Mozambique?
- 0.0081, with Armenia ahead.
- How many years of comparable data are there for Armenia and Mozambique?
- 64 years are reported by both, from 1960 to 2023.
- How do Armenia and Mozambique rank globally for standardised precipitation-evapotranspiration index?
- Armenia ranks 68th and Mozambique ranks 69th of 189 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.