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dc.contributor.authorGobin, Anne
dc.contributor.authorKersebaum, Kurt Christian
dc.contributor.authorEitzinger, Josef
dc.contributor.authorTrnka, Miroslav
dc.contributor.authorHlavinka, Petr
dc.contributor.authorTakác, Jozef
dc.contributor.authorKroes, Joop
dc.contributor.authorVentrella, Domenico
dc.contributor.authorMarta, Anna Dalla
dc.contributor.authorDeelstra, Johannes
dc.contributor.authorLalic, Branislava
dc.contributor.authorNejedlik, Pavol
dc.contributor.authorOrlandini, Simone
dc.contributor.authorPeltonen-Sainio, Pirjo
dc.contributor.authorRajala, Ari
dc.contributor.authorSaue, Triin
dc.contributor.authorSaylan, Levent
dc.contributor.authorStricevic, Ruzica
dc.contributor.authorVucetic, Visnja
dc.contributor.authorZoumides, Christos
dc.coverage.spatialEuropenb_NO
dc.date.accessioned2018-07-25T13:58:28Z
dc.date.available2018-07-25T13:58:28Z
dc.date.created2017-09-29T14:39:18Z
dc.date.issued2017-02-08
dc.identifier.citationWater. 2017, 9 (2), .nb_NO
dc.identifier.issn2073-4441
dc.identifier.urihttp://hdl.handle.net/11250/2506496
dc.description.abstractCrop growth and yield are affected by water use during the season: the green water footprint (WF) accounts for rain water, the blue WF for irrigation and the grey WF for diluting agri-chemicals. We calibrated crop yield for FAO’s water balance model “Aquacrop” at field level. We collected weather, soil and crop inputs for 45 locations for the period 1992–2012. Calibrated model runs were conducted for wheat, barley, grain maize, oilseed rape, potato and sugar beet. The WF of cereals could be up to 20 times larger than the WF of tuber and root crops; the largest share was attributed to the green WF. The green and blue WF compared favourably with global benchmark values (R2 = 0.64–0.80; d = 0.91–0.95). The variability in the WF of arable crops across different regions in Europe is mainly due to variability in crop yield (cv = 45%) and to a lesser extent to variability in crop water use (cv = 21%). The WF variability between countries (cv = 14%) is lower than the variability between seasons (cv = 22%) and between crops (cv = 46%). Though modelled yields increased up to 50% under sprinkler irrigation, the water footprint still increased between 1% and 25%. Confronted with drainage and runoff, the grey WF tended to overestimate the contribution of nitrogen to the surface and groundwater. The results showed that the water footprint provides a measurable indicator that may support European water governance.nb_NO
dc.description.abstractVariability in the Water Footprint of Arable Crop Production across European Regionsnb_NO
dc.language.isoengnb_NO
dc.publisherMDPI AG, Basel, Switzerlandnb_NO
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.subjectwater footprintnb_NO
dc.subjectarable cropsnb_NO
dc.subjectcerealsnb_NO
dc.subjectcrop water usenb_NO
dc.subjectyieldnb_NO
dc.titleVariability in the Water Footprint of Arable Crop Production across European Regionsnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionpublishedVersionnb_NO
dc.rights.holder© 2017 by the authors; licensee MDPI, Basel, Switzerlandnb_NO
dc.source.pagenumber22nb_NO
dc.source.volume9nb_NO
dc.source.journalWaternb_NO
dc.source.issue2nb_NO
dc.identifier.doi10.3390/w9020093
dc.identifier.cristin1500536
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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