New Zealand vs Togo: Standardised Precipitation-Evapotranspiration Index
Standardised Precipitation-Evapotranspiration Index over time
- New Zealand
- Togo
How they compare
New Zealand currently reports 0.469 against 0.4388 in Togo, a difference of 0.0302.
That makes New Zealand's figure about 1.1 times Togo's.
The two have swapped places 35 times across 64 shared years of data; in 1960 it was Togo ahead.
New Zealand ranks 35th and Togo ranks 36th of 189 countries.
Across the 7 decades both report, New Zealand averaged higher in 3 and Togo in 4.
Head to head by decade
| Decade | New Zealand | Togo | Difference | Ahead |
|---|---|---|---|---|
| 1960s | -0.1709 | 0.7042 | 0.8751 | Togo |
| 1970s | 0.2928 | 0.8306 | 0.5378 | Togo |
| 1980s | -0.1624 | 0.3082 | 0.4706 | Togo |
| 1990s | 0.2229 | 0.0919 | 0.1311 | New Zealand |
| 2000s | -0.4432 | -0.2686 | 0.1746 | Togo |
| 2010s | -0.1969 | -0.2131 | 0.0161 | New Zealand |
| 2020s | 0.6084 | -0.1754 | 0.7838 | New Zealand |
Averages of every year both report within each decade.
Frequently asked questions
- Which has higher standardised precipitation-evapotranspiration index, New Zealand or Togo?
- New Zealand, at 0.469 against 0.4388 in Togo as of 2023.
- What is the difference in standardised precipitation-evapotranspiration index between New Zealand and Togo?
- 0.0302, with New Zealand ahead.
- How many years of comparable data are there for New Zealand and Togo?
- 64 years are reported by both, from 1960 to 2023.
- How do New Zealand and Togo rank globally for standardised precipitation-evapotranspiration index?
- New Zealand ranks 35th and Togo ranks 36th 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.