194
In 2007, groundwater has been the most important source of water uses in the
Lower Jordan Basin. The total water abstraction for 2007 summed up to about
3131 × 10
6 m
3 . Israel released around 234 × 10
6 m
3 after use to the subsurface of
which 88 × 10
6 m
3 is lost due to leakages. Jordan released around 55 × 10
6 m
3 to
the subsurface with the share of losses probably being much higher as the unaccounted water in the municipals, which is around 50 % (Jordan Ministry for Water
and Irrigation 2009 ) and 30 % for the Palestine territories (Palestinian Water
Authority 2012 ).
13.1.2 Water Balance
The overall water balance for the region is presented in Fig. 13.4 . We calculated a
defi cit of around 280 × 10
6 m
3 in 2007 for the whole region.
10
142
152
126
495
621
691
1,631
2,322
3,425
50
−280
827
2,268
3,095
−500
0
500
1,000
1,500
2,000
2,500
3,000
3,500
4,000
Jordan
Israel + West Bank
Total
Total water
uses
Yarmouk River
inflow from Syria
Deficit
Recharges Jordan and Israel + West Bank
Total water uses, inflow Syria and Deficit
Volume [10
6
m
3
]
Desalinated water
Effluents
Average annual recharge
Total
Annual Water Balance for Israel, Westbank and Jordan Based on Data
from 2004 and 2007 (10 6 m/yr)
Fig. 13.4 Water balance for Israel, the West Bank and Jordan based on 2004 and 2007 data.
Source: According to Weinberger et al. ( 2012 , Table 4), the total average annual recharge for Israel
and the West Bank 1631 × 10
6 m
3 was calculated on a period from 1993 to 2009. 2007 data for
desalinated water and for effl uents were derived from Israel Central Bureau of Statistics ( 2012 ,
Table 7 and p. 20). For Jordan, we calculated the average annual recharge, the effl uents and the
amount of desalinated water on a very conservative basis, based on the data from the Jordan
National Master Plan from 2004 (Jordan Ministry for Water and Irrigation and German Technical
Cooperation 2004 , p. 48, Table 3.1 and p. 54) and from Water for Life (Jordan Ministry for Water
and Irrigation 2009 , executive summary, p. 7)
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