Bolivia vs Iceland: Standardised Precipitation-Evapotranspiration Index

Bolivia
0.2295
in 2023
Iceland
0.2221
in 2023
Bolivia rank
50th
Iceland rank
53rd

Standardised Precipitation-Evapotranspiration Index over time

  • Bolivia
  • Iceland
-202196019912023

How they compare

Bolivia currently reports 0.2295 against 0.2221 in Iceland, a difference of 0.0074.

The two have swapped places 18 times across 64 shared years of data; in 1960 it was Bolivia ahead.

Bolivia ranks 50th and Iceland ranks 53rd of 188 countries.

Across the 7 decades both report, Bolivia averaged higher in 1 and Iceland in 6.

Head to head by decade

Decade Bolivia Iceland Difference Ahead
1960s -1.38 -0.2499 1.13 Iceland
1970s 0.494 0.5134 0.0194 Iceland
1980s 0.9729 0.2356 0.7373 Bolivia
1990s -0.0072 0.6935 0.7008 Iceland
2000s 0.2189 0.8361 0.6172 Iceland
2010s -0.0576 0.9778 1.04 Iceland
2020s -1.15 0.8032 1.95 Iceland

Averages of every year both report within each decade.

Frequently asked questions

Which has higher standardised precipitation-evapotranspiration index, Bolivia or Iceland?
Bolivia, at 0.2295 against 0.2221 in Iceland as of 2023.
What is the difference in standardised precipitation-evapotranspiration index between Bolivia and Iceland?
0.0074, with Bolivia ahead.
How many years of comparable data are there for Bolivia and Iceland?
64 years are reported by both, from 1960 to 2023.
How do Bolivia and Iceland rank globally for standardised precipitation-evapotranspiration index?
Bolivia ranks 50th and Iceland ranks 53rd 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

Indicator
Standardised Precipitation-Evapotranspiration Index
Source
Global SPEI database (SPEIbase). https://spei.csic.es/database.html
Licence
CC BY 4.0 (World Bank Open Data)
Coverage
189 places, 12,095 data points, 1960–2023
Last refreshed

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.