Hungary vs Uganda: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- Hungary
- Uganda
How they compare
Hungary currently reports 0.3955 against 0.3376 in Uganda, a difference of 0.0579.
That makes Hungary's figure about 1.2 times Uganda's.
The two have swapped places 28 times across 64 shared years of data; in 1960 it was Hungary ahead.
Hungary ranks 40th and Uganda ranks 43rd of 188 countries.
Across the 7 decades both report, Hungary averaged higher in 1 and Uganda in 6.
Head to head by decade
| Decade | Hungary | Uganda | Difference | Ahead |
|---|---|---|---|---|
| 1960s | 0.1203 | 0.7094 | 0.5891 | Uganda |
| 1970s | 0.2043 | 0.2608 | 0.0565 | Uganda |
| 1980s | -0.1516 | -0.5199 | 0.3683 | Hungary |
| 1990s | -0.1029 | -0.0091 | 0.0938 | Uganda |
| 2000s | -0.6276 | -0.365 | 0.2626 | Uganda |
| 2010s | -0.5556 | 0.8989 | 1.45 | Uganda |
| 2020s | -0.9045 | 1.19 | 2.09 | Uganda |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, Hungary or Uganda?
- Hungary, at 0.3955 against 0.3376 in Uganda as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between Hungary and Uganda?
- 0.0579, with Hungary ahead.
- How many years of comparable data are there for Hungary and Uganda?
- 64 years are reported by both, from 1960 to 2023.
- How do Hungary and Uganda rank globally for standardised precipitation-evapotranspiration index?
- Hungary ranks 40th and Uganda ranks 43rd 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.