Datasets (2998)

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EDO Minimum Daily Temperature (version 1.0.0)

Daily interpolated minimum 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...

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EDO Maximum Temperature Anomaly (version 1.0.0)

Anomalies of maximum daily temperature are computed based on the interpolated maximum temperature data per day from 1981 and up to and including 2010. The temperature results are being used to compute heat- and cold waves and moments of potentially dangerous t...

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EDO Maximum Daily Temperature (version 1.0.0)

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...

Last updated: | Recent visits: 2
EDO Low Flow Index (LFI) (version 2.1.0)

The LFI indicator exploits the simulated 6-hours river water discharge outputs of the JRC’s in-house LISFLOOD hydrological model, in order to capture unbroken consecutive periods of unusually low streamflow, and compares the consequent water deficit during tho...

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EDO Soil Moisture Anomaly (SMA) (version 2.1.0)

Soil Moisture Anomaly (SMA) at 5-km spatial resolution, computed as standardized deviation from a baseline period 1995-2020. The dataset is derived from 6-hourly LISFLOOD modelled soil moisture in the top two soil layers, as produced for EFAS on a Lambert Azim...

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Digital Observatory For Protected Areas 4.1

The Digital Observatory for Protected Areas (DOPA) is a set of web services and applications that can be used primarily to assess, monitor, report and possibly forecast the state of and the pressure on protected areas at multiple scales. The data, indicators, ...

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11. Soil permeability

The European map of soil permeability displays the percentage of topsoil fine fraction (less than 63 micro m). It is possible to derive a rough estimation of the permeability very easily from the weight percentage of fine fraction.