Titlebook: Management of Shared Groundwater Resources; The Israeli-Palestin Eran Feitelson,Marwan Haddad Book 2001 Springer Science+Business Media New

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Overview of the Mountain Aquiferg along a north-south axis for some 150 km through Israel and the West Bank. The aquifer extends from the valleys of Yezre’el (Marj Bani Amr) and Beit She’an (Beisan), in the north, to near Beer Sheva (Beer Al-Sabeaa), in the south, and from under the Mediterranean coastal plain and the western foot

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The Need for Joint Management and Monitoring of the Water “Usage” Cyclery high population growth and the extreme need for development — as for irrigation, industrial or domestic use — results in full use of existing resources and in the pressing need for new sources. Also, the corresponding increase of waste products from industrial, domestic and agricultural activitie

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Legal and Administrative Responsibility of Domestic Water Supply to the Palestiniansboth now and in the future. The Israelis currently control the domestic water supply to the Palestinians, particularly in the West Bank. They supply 26.92 MCM yearly to the Palestinians in the West Bank, while the Palestinians themselves supply their Palestinian customers with 15.7 MCM yearly. The I

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Israeli-Palestinian Bargaining over the Mountain Aquifer Mountain Aquifer (MA). Because data availability for modeling the Israeli-Palestinian bargaining problem is limited, the simulation examines a broad range of economic circumstances that define the bargaining environment. That is, the effects of variations in these circumstances on the essential bar

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From Rights to Needsowever, application of an equitable water-sharing agreement along the volatile waterways of the globe is a prerequisite to hydropolitical stability. This paper explores the question of equity measures for water-sharing agreements in the context of global hydropolitics, describing the practice of wat

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Institutional Cooperation on Groundwater Issuesas, it is a permanently present in different shapes, describing ever again the hydrological cycle: it evaporates from the sea into clouds; it precipitates upon earth in the form of rain, snow or hail; it is assembled in groundwater or surface water; and, eventually, it flows back into sea. If human

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