Georgia vs Sweden: Standardised Precipitation-Evapotranspiration Index

Georgia
0.7379
in 2023
Sweden
0.7254
in 2023
Georgia rank
20th
Sweden rank
21st

Standardised Precipitation-Evapotranspiration Index over time

  • Georgia
  • Sweden
-2-10123196019912023

How they compare

Georgia currently reports 0.7379 against 0.7254 in Sweden, a difference of 0.0125.

The two have swapped places 31 times across 64 shared years of data; in 1960 it was Sweden ahead.

Georgia ranks 20th and Sweden ranks 21st of 188 countries.

Across the 7 decades both report, Georgia averaged higher in 2 and Sweden in 5.

Head to head by decade

Decade Georgia Sweden Difference Ahead
1960s 0.0174 0.1789 0.1615 Sweden
1970s -0.0068 -0.2924 0.2856 Georgia
1980s 0.3294 0.6478 0.3184 Sweden
1990s -0.0488 0.252 0.3008 Sweden
2000s 0.5349 0.4661 0.0688 Georgia
2010s -0.2643 0.3975 0.6618 Sweden
2020s -0.5389 0.0334 0.5723 Sweden

Averages of every year both report within each decade.

Frequently asked questions

Which has higher standardised precipitation-evapotranspiration index, Georgia or Sweden?
Georgia, at 0.7379 against 0.7254 in Sweden as of 2023.
What is the difference in standardised precipitation-evapotranspiration index between Georgia and Sweden?
0.0125, with Georgia ahead.
How many years of comparable data are there for Georgia and Sweden?
64 years are reported by both, from 1960 to 2023.
How do Georgia and Sweden rank globally for standardised precipitation-evapotranspiration index?
Georgia ranks 20th and Sweden ranks 21st 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.