Standardised Precipitation-Evapotranspiration Index in Luxembourg
Luxembourg: Standardised Precipitation-Evapotranspiration Index was 0.5375 in 2023. ◆ Volatile
Standardised Precipitation-Evapotranspiration Index in Luxembourg, 1960–2023
Source: Global SPEI database (SPEIbase). https://spei.csic.es/database.html.
Analysis
The most recent figure for standardised precipitation-evapotranspiration index in Luxembourg is 0.5375, measured in 2023.
Compared with earlier readings it is up 132.6% on the previous year and up 1,590.2% over ten years.
Over the whole period, standardised precipitation-evapotranspiration index in Luxembourg peaked at 2.71 in 1965 and was at its lowest, -2.12, in 1976.
Luxembourg ranks 28th of 189 countries on this measure, in the top quarter.
The series is highly variable year to year, so single readings are best treated with caution.
Standardised Precipitation-Evapotranspiration Index in Luxembourg, year by year
| Year | Value | Change |
|---|---|---|
| 1960 | 0.7441 | — |
| 1961 | 0.8406 | +13.0% |
| 1962 | 0.0557 | -93.4% |
| 1963 | -0.6327 | -1235.9% |
| 1964 | -1.14 | +79.4% |
| 1965 | 2.71 | -338.7% |
| 1966 | 2.21 | -18.5% |
| 1967 | 0.0038 | -99.8% |
| 1968 | 0.2828 | +7342.1% |
| 1969 | -0.3478 | -223.0% |
| 1970 | 0.7336 | -310.9% |
| 1971 | -1.57 | -314.0% |
| 1972 | -0.5277 | -66.4% |
| 1973 | -1 | +90.1% |
| 1974 | 1.26 | -225.4% |
| 1975 | -1.03 | -181.8% |
| 1976 | -2.12 | +106.4% |
| 1977 | 0.8336 | -139.3% |
| 1978 | 0.1 | -88.0% |
| 1979 | 1.1 | +1004.0% |
| 1980 | 1.05 | -4.4% |
| 1981 | 2.22 | +110.0% |
| 1982 | 0.0233 | -98.9% |
| 1983 | -0.0047 | -120.2% |
| 1984 | 1.28 | -27406.4% |
| 1985 | -0.5782 | -145.1% |
| 1986 | 0.8992 | -255.5% |
| 1987 | 1.46 | +62.0% |
| 1988 | 1.69 | +16.2% |
| 1989 | -0.8502 | -150.3% |
| 1990 | -0.6492 | -23.6% |
| 1991 | -1.32 | +103.5% |
| 1992 | -0.4005 | -69.7% |
| 1993 | 0.4107 | -202.5% |
| 1994 | 0.1043 | -74.6% |
| 1995 | 0.5789 | +455.0% |
| 1996 | -1.32 | -328.0% |
| 1997 | -0.5514 | -58.2% |
| 1998 | 0.8876 | -261.0% |
| 1999 | 0.7534 | -15.1% |
| 2000 | 1.07 | +41.4% |
| 2001 | 1.74 | +63.5% |
| 2002 | 1.22 | -30.2% |
| 2003 | -1.69 | -239.0% |
| 2004 | -0.2227 | -86.8% |
| 2005 | -0.8443 | +279.1% |
| 2006 | -0.3455 | -59.1% |
| 2007 | 0.5205 | -250.7% |
| 2008 | 0.0521 | -90.0% |
| 2009 | -0.6397 | -1327.8% |
| 2010 | 0.0963 | -115.1% |
| 2011 | -0.9877 | -1125.6% |
| 2012 | 0.3102 | -131.4% |
| 2013 | 0.0318 | -89.7% |
| 2014 | -0.5458 | -1816.4% |
| 2015 | -1.14 | +109.7% |
| 2016 | 0.1485 | -113.0% |
| 2017 | -0.5785 | -489.6% |
| 2018 | -1.6 | +176.9% |
| 2019 | -1 | -37.5% |
| 2020 | -1.28 | +28.4% |
| 2021 | 0.5582 | -143.4% |
| 2022 | -1.65 | -395.2% |
| 2023 | 0.5375 | -132.6% |
Luxembourg compared with similar countries
- Luxembourg's 0.5375 is above the median for high income countries, which is -0.3666. (63 countries reporting)
- Luxembourg's 0.5375 is above the median for Europe & Central Asia, which is -0.2017. (52 countries reporting)
Biggest year-on-year movements
Years where Standardised Precipitation-Evapotranspiration Index in Luxembourg 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 |
|---|---|---|---|
| 1984 | +27406.4% | -0.0047 | 1.28 |
| 1968 | +7342.1% | 0.0038 | 0.2828 |
| 2014 | -1816.4% | 0.0318 | -0.5458 |
| 2009 | -1327.8% | 0.0521 | -0.6397 |
| 1963 | -1235.9% | 0.0557 | -0.6327 |
Averages by decade
| Decade | Average | Lowest | Highest | Years |
|---|---|---|---|---|
| 1960s | 0.4728 | -1.14 | 2.71 | 10 |
| 1970s | -0.2225 | -2.12 | 1.26 | 10 |
| 1980s | 0.7192 | -0.8502 | 2.22 | 10 |
| 1990s | -0.1507 | -1.32 | 0.8876 | 10 |
| 2000s | 0.0854 | -1.69 | 1.74 | 10 |
| 2010s | -0.5272 | -1.6 | 0.3102 | 10 |
| 2020s | -0.4592 | -1.65 | 0.5582 | 4 |
Countries ranked near Luxembourg
More environment data for Luxembourg
- Historical exposure to drought — Land soil moisture anomaly -0.2585 Percentage change (2025)
- Historical exposure to drought — Cropland soil moisture anomaly -0.1872 Percentage change (2025)
- Standard Deviation, annual growth rate 0 % change on previous year (2025)
- Drought - Cities and FUAs — Land soil moisture anomaly -0.5 Percentage change (2025)
- Standard Deviation 0.601 °C (2025)
- Temperature change 2.18 °C (2025)
- Wood-based panels — Production, annual growth rate 0 % change on previous year (2024)
- Total greenhouse gas emissions excluding LULUCF (Mt CO2e), annual 2.56 % change on previous year (2024)
- Total greenhouse gas emissions excluding LULUCF (Mt CO2e), per unit 0 Mt CO2e per US$ of GDP (2024)
- Total greenhouse gas emissions excluding LULUCF (Mt CO2e), per capita 0 Mt CO2e per person (2024)
Frequently asked questions
- What is standardised precipitation-evapotranspiration index in Luxembourg?
- Standardised precipitation-evapotranspiration index in Luxembourg was 0.5375 in 2023, according to Global SPEI database (SPEIbase). https://spei.csic.es/database.html.
- What is the highest standardised precipitation-evapotranspiration index recorded in Luxembourg?
- The highest recorded value was 2.71 in 1965.
- What is the lowest standardised precipitation-evapotranspiration index recorded in Luxembourg?
- The lowest recorded value was -2.12 in 1976.
- How does Luxembourg rank for standardised precipitation-evapotranspiration index?
- Luxembourg ranks 28th out of 189 countries with data for 2023.
- Is standardised precipitation-evapotranspiration index rising or falling in Luxembourg?
- Over the last ten years it is up 1,590.2%. The long-run trend across the full record is volatile.
- Where does this Luxembourg 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.