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In Cisjordan, surface- and groundwater flow are either towards the Jordan Valley–Dead Sea–Arava Valley (the Rift) or the Mediterranean Sea. Due to upstream exploitation by riparians to the Jordan River, the historical annual flow, which fluctuated between 250 and 1100Mm 3 , has declined to a mere 100–200Mm 3 . The remaining flow south of Lake Kinneret is highly polluted and heavily...
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