http://www.passia.org/palestine_facts/MAPS/newpdf/Surface-Water.pdf

Nakolik se údaje palestinského zdroje liší od izraelských lze porovnat například na stránkách haifské univerzity zde:

http://research.haifa.ac.il/~eshkol/kantorb.html

Lake Kinneret covers an area of about 168 sq. km., containing 4 billion cu.m. of water. The lake receives most of its water from the Jordan, formed by the confluence of its three major tributaries; the Dan, which “contributes” some 250 million cu.m. per annum; the Snir (Hatsbani), with an average annual contribution of some 150 million cu.m., and the Hermon (Banias) River, contributing an annual average of about 120 cu.m. to the Jordan.
The Kinneret thus receives in an average year about 520 million cu.m. of water from its major tributaries. Together with minor tributaries, flood waters and other sources, the total average annual inflow into the Kinneret from its catchment basis amounts to about 850 million cu.m., 65% of which is from the Jordan and its tributaries, and 35% from all other sources. Some 300 million cu.m. of this water – evaporates.
About 500 million cu.m. of water is available for pumping from the Kinneret in an average year. Of this, about 400 million cu.m. is pumped into the National Water Carrier.

Národní přivaděč byl zprovozněn v r 1964, Syřané začali budovat bypas mezi horním a dolním tokem Jordánu v r 1965. Obsazením Golan v r.1967 se vše tak nějak vyřešilo. Výsledkem je, že do Mrtvého moře vtékají de facto vody Jarmůku a ne vody Jordánu. A celá Západní obora je závislá na Mekorotu, protože i kdyby měla přístup k tomu co bylo “Jordánem” není z něj pomalu co cucat.