Metadata 1658
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
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 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
Zones inside groundwater bodies or groundwater bodies potentially leading to operational problems for shallow geothermal use due to a critical chemical composition.
A Talajvíztükör NATéR témakörhöz tartozó térképsorozat.
Polish Geological Institute - National Research Institute (PGI-NRI) provides measurement results, tests in terms of quality and amount of groundwater, necessary for quantitative and chemical assessment of groundwater. The organisation and scope of groundwater monitoring was adapted to comply with European Community directives, particularly the Water Framework Directive (2000/60/EC), Groundwater Directive (2006/118/EC) and Nitrates Directive (91/676/EEC), in accordance with its specific features resulting f...
Areas dedicated to drinking water or curative water supply, which might limit the use of shallow geothermal energy.
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 coefficie...
A dataset used to display the intrinsic geological and hydrogeological characteristics that determine the ease with which groundwater may be contaminated by human activities.