Kiribati vs Lebanon: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Kiribati
- Lebanon
How they compare
Lebanon currently reports 0.2115 against 0.1953 in Kiribati, a difference of 0.0162.
That makes Lebanon's figure about 1.1 times Kiribati's.
The two have swapped places 27 times across 64 shared years of data; in 1960 it was Kiribati ahead.
Kiribati ranks 55th and Lebanon ranks 54th of 189 countries.
Across the 7 decades both report, Kiribati averaged higher in 4 and Lebanon in 3.
Head to head by decade
| Decade | Kiribati | Lebanon | Difference | Ahead |
|---|---|---|---|---|
| 1960s | -0.5955 | 0.1848 | 0.7803 | Lebanon |
| 1970s | -0.1076 | 0.1028 | 0.2104 | Lebanon |
| 1980s | 0.0112 | 0.1336 | 0.1225 | Lebanon |
| 1990s | 0.0004 | -0.2682 | 0.2686 | Kiribati |
| 2000s | 0.1965 | -0.3095 | 0.506 | Kiribati |
| 2010s | 0.2008 | -0.3806 | 0.5814 | Kiribati |
| 2020s | 0.1868 | -0.1012 | 0.288 | Kiribati |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Kiribati or Lebanon?
- Lebanon, at 0.2115 against 0.1953 in Kiribati as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Kiribati and Lebanon?
- 0.0162, with Lebanon ahead.
- How many years of comparable data are there for Kiribati and Lebanon?
- 64 years are reported by both, from 1960 to 2023.
- How do Kiribati and Lebanon rank globally for standardised precipitation-evapotranspiration index?
- Kiribati ranks 55th and Lebanon ranks 54th 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.