Standardised Precipitation-Evapotranspiration Index in Andorra
Andorra: Standardised Precipitation-Evapotranspiration Index was -2.17 in 2023. ◆ Volatile
Standardised Precipitation-Evapotranspiration Index in Andorra, 1960–2023
Source: Global SPEI database (SPEIbase). https://spei.csic.es/database.html.
Analysis
In 2023, standardised precipitation-evapotranspiration index in Andorra stood at -2.17. That is the lowest value across all 64 years on record.
The figure is down 13.7% on the previous year and down 606.6% over ten years.
Over the whole period, standardised precipitation-evapotranspiration index in Andorra peaked at 1.96 in 1960 and was at its lowest, -2.17, in 2023.
Andorra ranks 184th of 189 countries on this measure, in the bottom quarter.
The series is highly variable year to year, so single readings are best treated with caution.
Standardised Precipitation-Evapotranspiration Index in Andorra, year by year
| Year | Value | Change |
|---|---|---|
| 1960 | 1.96 | — |
| 1961 | -0.4458 | -122.7% |
| 1962 | 1.3 | -391.5% |
| 1963 | 1.74 | +33.9% |
| 1964 | 1.08 | -37.8% |
| 1965 | 1.02 | -5.5% |
| 1966 | 0.6572 | -35.7% |
| 1967 | 0.0294 | -95.5% |
| 1968 | 0.7152 | +2332.7% |
| 1969 | 1.3 | +82.3% |
| 1970 | -0.0527 | -104.0% |
| 1971 | 1.31 | -2589.8% |
| 1972 | 1.71 | +30.2% |
| 1973 | -0.2088 | -112.2% |
| 1974 | 0.7624 | -465.1% |
| 1975 | 0.4674 | -38.7% |
| 1976 | 0.1187 | -74.6% |
| 1977 | 1.41 | +1090.6% |
| 1978 | -0.2711 | -119.2% |
| 1979 | 1.53 | -665.9% |
| 1980 | -0.2669 | -117.4% |
| 1981 | 0.64 | -339.8% |
| 1982 | 1.53 | +139.2% |
| 1983 | -0.404 | -126.4% |
| 1984 | 0.4526 | -212.0% |
| 1985 | -1.46 | -422.3% |
| 1986 | -1.35 | -7.4% |
| 1987 | 0.8753 | -164.8% |
| 1988 | -0.0252 | -102.9% |
| 1989 | -0.5945 | +2259.1% |
| 1990 | -0.293 | -50.7% |
| 1991 | -0.6837 | +133.3% |
| 1992 | 1.58 | -331.8% |
| 1993 | -0.6471 | -140.8% |
| 1994 | -0.0583 | -91.0% |
| 1995 | -0.1299 | +122.8% |
| 1996 | 1.79 | -1480.7% |
| 1997 | 0.8312 | -53.7% |
| 1998 | -1.4 | -268.4% |
| 1999 | 0.3227 | -123.1% |
| 2000 | -0.674 | -308.9% |
| 2001 | -0.8655 | +28.4% |
| 2002 | 0.6614 | -176.4% |
| 2003 | 0.4907 | -25.8% |
| 2004 | -1.19 | -342.6% |
| 2005 | -1.54 | +29.2% |
| 2006 | -1.67 | +8.6% |
| 2007 | -1.85 | +10.7% |
| 2008 | 0.629 | -134.0% |
| 2009 | -0.306 | -148.6% |
| 2010 | 0.2336 | -176.3% |
| 2011 | -1.16 | -598.2% |
| 2012 | -1.49 | +27.6% |
| 2013 | 0.4285 | -128.9% |
| 2014 | 0.5108 | +19.2% |
| 2015 | -1.38 | -370.2% |
| 2016 | -1.23 | -11.0% |
| 2017 | -1.22 | -0.3% |
| 2018 | 1.42 | -216.3% |
| 2019 | -0.8881 | -162.3% |
| 2020 | 0.1959 | -122.1% |
| 2021 | -1.33 | -781.2% |
| 2022 | -1.91 | +43.1% |
| 2023 | -2.17 | +13.7% |
Andorra compared with similar countries
- Andorra's -2.17 is below the median for high income countries, which is -0.3666, 5.9× the median. (63 countries reporting)
- Andorra's -2.17 is below the median for Europe & Central Asia, which is -0.2017, 10.8× the median. (52 countries reporting)
Biggest year-on-year movements
Years where Standardised Precipitation-Evapotranspiration Index in Andorra changed far more than this series normally does. A large move can be a real event or a change in how the figure was measured — the source note below says who published it.
| Year | Change | From | To |
|---|---|---|---|
| 1971 | +2589.8% | -0.0527 | 1.31 |
| 1968 | +2332.7% | 0.0294 | 0.7152 |
| 1989 | -2259.1% | -0.0252 | -0.5945 |
| 1996 | +1480.7% | -0.1299 | 1.79 |
| 1977 | +1090.6% | 0.1187 | 1.41 |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1960s | 0.9369 | -0.4458 | 1.96 | 10 |
| 1970s | 0.6784 | -0.2711 | 1.71 | 10 |
| 1980s | -0.0601 | -1.46 | 1.53 | 10 |
| 1990s | 0.1321 | -1.4 | 1.79 | 10 |
| 2000s | -0.631 | -1.85 | 0.6614 | 10 |
| 2010s | -0.4773 | -1.49 | 1.42 | 10 |
| 2020s | -1.3 | -2.17 | 0.1959 | 4 |
Countries ranked near Andorra
More environment data for Andorra
- Standard Deviation, annual growth rate 0 % change on previous year (2025)
- Historical exposure to drought — Land soil moisture anomaly -1.28 Percentage change (2025)
- Historical exposure to drought — Cropland soil moisture anomaly -1.18 Percentage change (2025)
- Standard Deviation 0.417 °C (2025)
- Temperature change 2.58 °C (2025)
- Cropland — Area per capita 0 ha/cap (2024)
- Land area — Area 46.8 1000 ha (2024)
- Cropland — Share in Land area 0.31 % (2024)
- Cropland — Share in Agricultural land 0.74 % (2024)
- Cropland — Area 0.1443 1000 ha (2024)
Frequently asked questions
- What is standardised precipitation-evapotranspiration index in Andorra?
- Standardised precipitation-evapotranspiration index in Andorra was -2.17 in 2023, according to Global SPEI database (SPEIbase). https://spei.csic.es/database.html.
- What is the highest standardised precipitation-evapotranspiration index recorded in Andorra?
- The highest recorded value was 1.96 in 1960.
- What is the lowest standardised precipitation-evapotranspiration index recorded in Andorra?
- The lowest recorded value was -2.17 in 2023.
- How does Andorra rank for standardised precipitation-evapotranspiration index?
- Andorra ranks 184th out of 189 countries with data for 2023.
- Is standardised precipitation-evapotranspiration index rising or falling in Andorra?
- Over the last ten years it is down 606.6%. The long-run trend across the full record is volatile.
- Where does this Andorra data come from?
- The figures come from Global SPEI database (SPEIbase). https://spei.csic.es/database.html, published as part of Standardised Precipitation-Evapotranspiration Index. Statizoid updates them automatically from the source API.
Download this data
CSV · JSON — 64 observations, free to reuse under CC BY 4.0 (World Bank Open Data).
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.