000189596 001__ 189596 000189596 005__ 20200702121727.0 000189596 0247_ $$2doi$$a10.1007/s00767-014-0280-6 000189596 0247_ $$2ISSN$$a1430-483X 000189596 0247_ $$2ISSN$$a1432-1165 000189596 0247_ $$2WOS$$aWOS:000351399600004 000189596 037__ $$aFZJ-2015-02734 000189596 082__ $$a690 000189596 1001_ $$0P:(DE-HGF)0$$aGörlich, Isa$$b0$$eCorresponding Author 000189596 245__ $$aStatusanalyse von Meerwasserintrusionen und Grundwasserhaushaltsmodellierung des oberen Küstenaquifers in Agadir, MarokkoStatusanalysis and groundwater storage model of the upper coastal aquifer in Agadir, Morocco 000189596 260__ $$aBerlin$$bSpringer$$c2015 000189596 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1429615521_14033 000189596 3367_ $$2DataCite$$aOutput Types/Journal article 000189596 3367_ $$00$$2EndNote$$aJournal Article 000189596 3367_ $$2BibTeX$$aARTICLE 000189596 3367_ $$2ORCID$$aJOURNAL_ARTICLE 000189596 3367_ $$2DRIVER$$aarticle 000189596 520__ $$aIn Agadir, a coastal town situated in the semi-arid south-western part of Morocco, irrigated agriculture and tourism are the primary economic activities. Both sectors require high volumes of fresh water. Over the last few decades, this constantly increasing demand has resulted in a significant drawdown of the water table, accompanied by seawater intrusion leading to a decrease in water quality. A groundwater storage model has verified the extensive drawdown. Positive terms in the flow balance equation are represented by groundwater recharge from bankfiltration, and by irrigation return flow. The negative terms are dominated by groundwater removal for irrigation. A sensitivity analysis reveals parameters which require further investigation. A spatially and temporally variable seawater intrusion front was identified using specific ion ratios, chloride concentrations and groundwater salinity. The intrusion front extends roughly from the northwest to the southeast, following the coast. Compared to 2005, the intrusion front had advanced further inland by 2010. 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