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Dashboard (Tableau)

Soil moisture

Dashboard (Tableau)
Prod-ID: DAS-223-en
Published 13 Aug 2020
1 min read
Monitoring soil moisture shortages is a precondition for managing drought adaptation and resilience of ecosystems, such as foreseen by the EU Nature restoration plan of the EU Biodiversity strategy 2030. This dashboard analyses 20 years (2000-2019) soil moisture content in Europe (EU27, EEA-38 and the UK). Soil moisture deficits, trends in soil moisture values and the area under pressure are presented by countries and land cover. Scroll down to the More information section for further details.

More information

Access the annual growing season soil moisture dataset here:

https://www.eea.europa.eu/data-and-maps/data/soil-moisture-deficit-during-the  

Soil moisture is essential for the development of plants, it regulates soil structure, soil temperature, salinity and the presence of toxic substances and it contributes to prevent soil erosion. As it determines conditions for land use, soil moisture content is an important element of the land system.

Soil moisture is measured in standardised anomalies, i.e. in standard deviations from the long-term (1995-2019) normal conditions. Negative values indicate deficit in soil moisture content whereas positive values indicate more than average soil moisture content. 

Soil moisture time series is acquired through the Copernicus Emergency Service maintained by the Joint Research Center of the European Commission.

 

More info:

https://edo.jrc.ec.europa.eu/documents/factsheets/factsheet_soilmoisture.pdf

https://edo.jrc.ec.europa.eu/edov2/php/index.php?id=1000 

 

Related content

Based on data

Data Soil moisture deficit during the vegetation growing season, annual time-series, 2000-2019 The dataset consists of a collection of annual soil moisture (SM) anomalies during the vegetation growing season (GS) for the years 2000-2019 across EEA 38 area and the United Kingdom. The vegetation growing season is defined by EEA´s phenology data series "Vegetation growing season length 2000-2016" [https://www.eea.europa.eu/data-and-maps/data/annual-above-ground-vegetation-season]. The anomalies are calculated based on the European Commission's Joint Research Centre European Drought Observatory (EDO) Soil Moisture Index (SMI) with respect to the 1995–2019 base period. The yearly start and end of GS periods are dynamic and calculated according to the EEA Phenology Indicators. A positive anomaly indicates that the observed SM was wetter than the long-term SM average for the base period, while a negative anomaly indicates that the observed SM was drier than the reference value. Because SM anomalies are measured in units of standard deviation from the long-term SMI average, they can be used to compare annual deficits/surplus of SM between geographic regions. EDO is one of the early warning and monitoring systems of the Copernicus Emergency Management Service. As the dataset builds on EDO's SMI, it therefore contains modified Copernicus Emergency Management Service information (2019).

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Temporal coverage

For references, please go to https://www.eea.europa.eu/data-and-maps/data/data-viewers/soil-moisture or scan the QR code.

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