60eff98f-5230-481d-92d1-3de80a010833 eng utf8 dataset Deltares Netherlands Eva.Schoonderwoerd@deltares.nl pointOfContact 2025-01-16 ISO 19115/INSPIRE_TG2/CZ4 2003/cor.1/2006 ETRS-LAEA (3035) [INSPIRE] Local - depth National scale potential recharge values for the Netherlands 2021-01-15 creation Version 1.0 netherlands_ltarech_1980_2010 modelDigital A national scale map that shows yearly LTA potential recharge values (mm/year) calculated over the Netherlands. Values are averaged over the period 1981 to 2010 Deltares Netherlands Eva.Schoonderwoerd@deltares.nl custodian Hydrography Geology GEMET - INSPIRE themes, version 1.0 2008-06-01 publication National Spatial scope 2019-05-22 publication Location of water bodies INSPIRE priority data set 2018-04-04 publication recharge national water budget resource resource management GeoERA Keyword Thesaurus 2020-01-01 publication TACTIC European Geoscience Registry - Projects 2020-01-01 publication Groundwater; Potential recharge; NrtGreat Britain; Long term average; otherRestrictions Creative Commons BY 4.0 Copyright (All Rigths Reserved) Please contact https://www.deltares.nl otherRestrictions public access limited according to Article 13(1)(a) of the INSPIRE Directive Please contact https://www.deltares.nl grid eng environment 3.358 7.227 50.751 53.554 Netherlands 0.01 8 TIFF 10.3 https://maps.europe-geology.eu/?mapname=tactic_preview#layers=netherlands_ltarech_1980_2010 WWW:LINK-1.0-http--link EGDI platform information Commission Regulation (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services 2010-12-08 See referenced specification Lineage (How data are created and model is calibrated): Recharge values are calculated using the Netherlands Hydrological Instrument (NHI). NHI is an integrated model including groundwater, surfacewater, and the vadose zone, using a a spatial resolution of 250 m and a temporal resolution of 1 day (De Lange et al, 2014). The model is forced by climate parameters as provided by the Dutch Meteorological institute. Recharge values are verified as they produce acceptable water balance when used to drive the national scale numerical groundwater flow simulator.