000889130 001__ 889130 000889130 005__ 20230418141423.0 000889130 0247_ $$2doi$$a10.1007/s00767-020-00471-x 000889130 0247_ $$2ISSN$$a1430-483X 000889130 0247_ $$2ISSN$$a1432-1165 000889130 0247_ $$2Handle$$a2128/27398 000889130 0247_ $$2WOS$$aWOS:000605146100001 000889130 037__ $$aFZJ-2021-00055 000889130 041__ $$aGerman 000889130 082__ $$a550 000889130 1001_ $$0P:(DE-Juel1)141774$$aHerrmann, Frank$$b0$$eCorresponding author 000889130 245__ $$aMit der Modellkette RCP-GCM-RCM-mGROWA projizierte Grundwasserneubildung als Datenbasis für zukünftiges Grundwassermanagement in Nordrhein-Westfalen Groundwater recharge in North Rhine-Westphalia projected using the model chain RCP-GCM-RCM-mGROWA 000889130 260__ $$aHeidelberg$$bSpringer$$c2021 000889130 3367_ $$2DRIVER$$aarticle 000889130 3367_ $$2DataCite$$aOutput Types/Journal article 000889130 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1639038153_6863 000889130 3367_ $$2BibTeX$$aARTICLE 000889130 3367_ $$2ORCID$$aJOURNAL_ARTICLE 000889130 3367_ $$00$$2EndNote$$aJournal Article 000889130 520__ $$aIn order to analyze the impact of climate change on groundwater resources in North Rhine-Westphalia a multi-model ensemble for projecting future groundwater recharge was established. The ensemble consists of 36 members of the model chain RCP-GCM-RCM-mGROWA in total, i.e. combinations of 3 greenhouse gas concentration trajectories, 6 global and 5 regional climate models, and the water balance model mGROWA. The ensemble projections show only a few significant changes of groundwater recharge in the future periods 2011–2040, 2041–2070, and 2071–2100. A robustness test using the two-criteria model agreement and the significance of the individual model projections did not reveal systematic and significant changes of groundwater recharge until 2100. From the statistical point of view, groundwater recharge can be expected to remain at the current level. 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