Kyrgyzstan vs San Marino: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Kyrgyzstan
- San Marino
How they compare
San Marino currently reports -1.16 against -1.16 in Kyrgyzstan, a difference of 0.
The two have swapped places 38 times across 64 shared years of data; in 1960 it was San Marino ahead.
Kyrgyzstan ranks 151st and San Marino ranks 150th of 189 countries.
Across the 7 decades both report, Kyrgyzstan averaged higher in 6 and San Marino in 1.
Head to head by decade
| Decade | Kyrgyzstan | San Marino | Difference | Ahead |
|---|---|---|---|---|
| 1960s | 0.2749 | 0.2563 | 0.0186 | Kyrgyzstan |
| 1970s | -0.0518 | 0.5166 | 0.5684 | San Marino |
| 1980s | 0.3433 | 0.2903 | 0.0529 | Kyrgyzstan |
| 1990s | 0.4365 | 0.1573 | 0.2792 | Kyrgyzstan |
| 2000s | 0.0891 | 0.0525 | 0.0366 | Kyrgyzstan |
| 2010s | 0.0179 | -0.7273 | 0.7452 | Kyrgyzstan |
| 2020s | -0.5481 | -1.62 | 1.07 | Kyrgyzstan |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Kyrgyzstan or San Marino?
- San Marino, at -1.16 against -1.16 in Kyrgyzstan as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Kyrgyzstan and San Marino?
- 0, with San Marino ahead.
- How many years of comparable data are there for Kyrgyzstan and San Marino?
- 64 years are reported by both, from 1960 to 2023.
- How do Kyrgyzstan and San Marino rank globally for standardised precipitation-evapotranspiration index?
- Kyrgyzstan ranks 151st and San Marino ranks 150th 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.