Daily minimum temperature exceedance over the 90th-percentile climatological daily minimum temperature, calculated from ERA5 temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 0.25 decimal degrees.

Daily maximum temperature exceedance over the 90th-percentile climatological daily maximum temperature, calculated from ERA5 temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 0.25 decimal degrees.

Daily maximum temperature exceedance over the 10th-percentile climatological daily maximum temperature, calculated from ERA5 temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 0.25 decimal degrees.

Daily minimum temperature exceedance over the 10th-percentile climatological daily minimum temperature, calculated from ERA5 temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 0.25 decimal degrees.

The Low-Flow Index (LFI) is based on the simulated 6-hours river discharge computed with LISFLOOD OS hydrological model, in order to capture unbroken consecutive periods of unusually low streamflow, and compares the consequent water deficit during those period...

Accumulated cold-wave intensity in degrees Celsius (°C) in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Daily minimum near-surface temperature in degrees Celsius (°C). Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Daily maximum near-surface temperature in degrees Celsius (°C). Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Duration in days of a cold-wave event in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Duration in days of a heat-wave event in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Accumulated heat-wave intensity in degrees Celsius (°C) in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees.

Soil Moisture Anomaly (SMA) at 1 arcmin spatial resolution, computed as standardized deviation from a baseline period 1995-2024. The dataset is derived from 6-hourly LISFLOOD modelled soil moisture in the top two soil layers, as produced for EFAS5.

Average root zone Soil Moisture Index (SMI) at 1 arcmin spatial resolution. The dataset is derived from 6-hourly LISFLOOD modelled soil moisture in the top two soil layers, as produced for EFAS5.

The Snow Masks used in the European Drought Observatory (EDO) are a collection of time-varying binary spatial layers (one for each 10-day period of the year) used to depict the location and extent of snow on the ground. The input data for calculating the snow...

The 9-month Standardized Precipitation Index (SPI-9) is a meteorological drought indicator to monitor precipitation anomalies over 9-month accumulation periods and is a proxy indicator for medium-term impacts, for example reduced stream flow and reservoir stor...

The 48-month Standardized Precipitation Index (SPI-48) is a meteorological drought indicator to monitor precipitation anomalies over 48-month accumulation periods and is a proxy indicator for long-term impacts, for example, reduced reservoir and groundwater re...

The 6-month Standardized Precipitation Index (SPI-6) is a meteorological drought indicator to monitor precipitation anomalies over 6-month accumulation periods and is a proxy indicator for medium-term impacts, for example reduced stream flow and reservoir stor...

The 3-month Standardized Precipitation Index (SPI-3) is a meteorological drought indicator to monitor precipitation anomalies over 3-month accumulation periods and is a proxy indicator for immediate impacts of droughts, such as reduced soil moisture, snowpack,...

The 24-month Standardized Precipitation Index (SPI-24) is a meteorological drought indicator to monitor precipitation anomalies over 24-month accumulation periods and is a proxy indicator for long-term impacts, for example, reduced reservoir and groundwater re...