Simulated change in mean groundwater head between the future (1 degree warming, minimum precipitation change) and past (2015) for the Upper Guadiana Basin, Spain. Simulated by a 1000 m by 1000 m grid. Unit: Meters.

The layers provide information on the intensity of mobile fishing associated with Oil and Gas pipelines and cables. Each layer was created by calculating the total number of fishing tracks in 1 km by 1 km squares along the length of each pipeline for four gear categories (see Rouse et al 2017). Fishing tracks were recreated for UK vessels greater than 15 m in length between 2007-2015 operating mobile demersal gear (otter trawls, pair trawls, beam trawlers and dredges) using vessel position data extracted from the Vessel Monitoring System. The layers can be used to aid the pipeline decommissioning process, including assessing the potential impacts and risks of different decommissioning options to commercial fisheries and informing the frequency of post-decommissioning monitoring according to level of fisheries interaction. The layers can also inform risk modelling for operational pipelines.

Long term average (LTA) Potential Groundwater Recharge (GWRpot) for the European domain at 1 km spatial resolution for the period 1981-2010. The LTA GWRpot data set i part of a series of gridded datasets established in the TACTIC project for estimating Potential Groundwater Recharge (GWRpot). The data available are AET, Effective precipitation (Peff=Precipitation-AET), Groundwater Recharge coefficient (Rcoef defined as the ratio: Peff / GWRpot ) The Potential Groundwater Recharge GWRpot = (Precipitation-AET)*Rcoef. The TACTIC series of gridded datasets for estimation of GWRpot included two versions of GWRpot. The current dataset is the GWRpot_biacorr= Peff_biascorr*Rcoef, adjusted to other Peff estimates from seven national pilots in Europe. The other is GWRpot =Peff*Rcoef. Urban areas are masked out and not represented in the gridded dataset. All units are mm/year for the period 1981-2010.

Groundwater Recharge Coefficient (Rcoef) for the European domain at 1 km spatial resolution for the period 1981-2010. The Rcoef estimate is based on a machine learning approach trained against gridded Rcoef estimates from seven national pilots in Europe. The Rcoef data set i part of a series of gridded datasets established in the TACTIC project for estimating Potential Groundwater Recharge (GWRpot). The data available are AET, Effective precipitation (Peff=Precipitation-AET), Groundwater Recharge coefficient (Rcoef defined as the ratio: Peff / GWRpot ) The Potential Groundwater Recharge GWRpot = (Precipitation-AET)*Rcoef. . Urban areas are masked out and not represented in the gridded dataset. Rcoef is a unitless ratio representing the period 1981-2010.

Long term average (LTA) Effective Precipitation (Peff) for the European domain at 1 km spatial resolution for the period 1981-2010. The Peff estimate is based on E-Obs precipitation records and a merged AET estimate based on the Budyko method and satellite estimates. The LTA Peff data set i part of a series of gridded datasets established in the TACTIC project for estimating Potential Groundwater Recharge (GWRpot). The data available are AET, Effective precipitation (Peff=Precipitation-AET), Groundwater Recharge coefficient (Rcoef defined as the ratio: Peff / GWRpot ) The Potential Groundwater Recharge GWRpot = (Precipitation-AET)*Rcoef. The TACTIC series of gridded datasets for estimation of GWRpot included two versions of Peff. The current dataset is the Peff_biacorr= (Precipitation-AET)*1.26, adjusted to other Peff estimates from seven national pilots in Europe. The other is Peff = Precipitation-AET. Urban areas are masked out and not represented in the gridded dataset. All units are mm/year for the period 1981-2010.

Simulated change in mean groundwater head between the future (1 degree warming, minimum precipitation change) and past (1980-2010) for Boutonne, France. Simulated by a 1000 m by 1000 m grid. Unit: Meters.

Simulated change in mean groundwater head between the future (3 degree warming, maximum precipitation change) and past (1980-2010) for Boutonne, France. Simulated by a 1000 m by 1000 m grid. Unit: Meters.

The difference in groundwater levels calculated by the hydrodynamic model in m between 2071-2100 and 1975-2004; RCA4/CNRM-CM5/RCP8.5 climate model. Simulated by a 2000 m by 2000 m grid, resolution: 1000 m by 1000 m grid. Unit: Meters. In the frame of NATeR - NAGIS, https://map.mbfsz.gov.hu

The difference in groundwater levels calculated by the hydrodynamic model in m between 2071-2100 and 1975-2004; RCA4/CNRM-CM5/RCP4.5 climate model. Simulated by a 2000 m by 2000 m grid, resolution: 1000 m by 1000 m grid. Unit: Meters. In the frame of NATeR - NAGIS, https://map.mbfsz.gov.hu

The difference in groundwater levels calculated by the hydrodynamic model in m between 2023-2052 and 1975-2004; RCA4/CNRM-CM5/RCP8.5 climate model. Simulated by a 2000 m by 2000 m grid, resolution: 1000 m by 1000 m grid. Unit: Meters. In the frame of NATeR - NAGIS, https://map.mbfsz.gov.hu