Daily minimum temperature exceedance over the 90th-percentile climatological daily minimum temperature, calculated from MARSMet temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 10 kilometres.

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

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

Daily maximum temperature exceedance over the 90th-percentile climatological daily maximum temperature, calculated from MARSMet temperature data. Temperature in degrees Celsius (°C). Spatial resolution: 10 kilometres.

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 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 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 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.

Accumulated warm spell 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. Important remark: in common language, extreme temperature events are usually...

Duration in days of a warm spell event in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees. Important remark: in common language, extreme temperature events are usually referred to as He...

Duration in days of a cold spell event in any given day as defined by the temperature anomalies method. Based on ERA5 data. Spatial resolution: 0.25 decimal degrees. Important remark: in common language, extreme temperature events are usually referred to as He...

Accumulated cold spell 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. Important remark: in common language, extreme temperature events are usually...

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...

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.

The Risk of Drought Impacts for Agriculture (RDrI-Agri) indicator that is implemented in the Global Drought Observatory (GDO) of the Copernicus Emergency Management Service, is used for determining the area more likely to be affected by droughts. Higher risk m...

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 Combined Drought Indicator (CDI) is an indicator for drought early warning, specifically designed to monitor agricultural drought. Through the combination of spatial patterns of precipitation, soil moisture and greenness vegetation anomalies, the CDI ident...

Daily interpolated maximum temperature using around 4000 weather stations across Europe and its surrounding areas. The data are interpolated using an inverse distance algorithm searching stations within 200 km distance. Up to a maximum of 20 stations are consi...