climate change on UAE - Stockholm Environment Institute-US Center
climate change on UAE - Stockholm Environment Institute-US Center
climate change on UAE - Stockholm Environment Institute-US Center
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including estimates of populati<strong>on</strong> and percapita<br />
demand.<br />
The average per capita domestic demand is<br />
estimated at 525 to 600 l/cap/day, with network<br />
losses of about 25%. In some areas, where the<br />
populati<strong>on</strong> uses water for irrigating the green<br />
areas around Villas, this average c<strong>on</strong>sumpti<strong>on</strong><br />
can grown to more than 1000 l/cap/day. This<br />
is a very high rate of use, with <strong>US</strong>A use rates<br />
of about 300 l/cap/day and Europe 125, l/cap/<br />
day. By simply multiplying per capita use by<br />
populati<strong>on</strong>, the total residential water use in<br />
2003 was about 280 Mm 3 , which represents<br />
about 45% of the desalinized water use.<br />
Government and commercial use another 45%<br />
and outdoor watering of gardens the remaining<br />
10% of desalinized water. To reflect government,<br />
commercial, and other outdoor uses, we have<br />
simply doubled per capita use to 1100 and 900<br />
l/cap/day in the western and eastern regi<strong>on</strong>s,<br />
respectively.<br />
In this table, per capita c<strong>on</strong>sumpti<strong>on</strong> reflects<br />
just residential uses and is estimated simply<br />
as the product of populati<strong>on</strong> and per-capita<br />
water use estimates. Government, schools,<br />
and commercial uses are assumed to double<br />
this rate (Abu Dhabi Water and Electricity,<br />
Regulati<strong>on</strong> and Supervisi<strong>on</strong> Bureau). The<br />
per-capita c<strong>on</strong>sumpti<strong>on</strong> rate is doubled in the<br />
WEAP model to reflect all M&I uses.<br />
When different outdoor demands are served<br />
by different supply sources or have different<br />
priorities, another ‘Green Circle’ is introduced<br />
into the model. These catchment nodes (Figure<br />
4-1 inset; green dots) represent land cover water<br />
demands, including outdoor irrigati<strong>on</strong>. For<br />
example, the Abu Dhabi Irg node represents<br />
the outdoor amenity water and agricultural<br />
irrigati<strong>on</strong> for the commodities represented in<br />
the model. The ‘Green Dot’ labeled 'Al Whathba'<br />
Forest represents the planted trees outside the<br />
main municipal area, which receive the same<br />
sources of water as the 'Abu Dhabi Irg' but have<br />
a lower priority (Priority 2) for receiving water.<br />
In times of shortage, Abu Dhabi Irg will receive<br />
water before Al Whathba Forest.<br />
Data attributes for the catchment model objects<br />
include representative area; irrigati<strong>on</strong> timing<br />
and efficiency, and climatically driven potential<br />
evapotranspirati<strong>on</strong>. Irrigati<strong>on</strong> demands are<br />
calculated using the standard United Nati<strong>on</strong>s<br />
Food and Agricultural Organizati<strong>on</strong> (FAO)<br />
method summarized in Crop evapotranspirati<strong>on</strong><br />
- Guidelines for computing crop water<br />
requirements (Allen et al. 1998).<br />
The WEAP representati<strong>on</strong> of the eastern<br />
regi<strong>on</strong> of Abu Dhai Emirate is shown in the<br />
figure above Figure 4-2, and includes several<br />
municipal/industrial demand nodes (e.g.,<br />
Swehan, Al Shoosh and Al-Ain); and catchment<br />
nodes representing irrigati<strong>on</strong> demands (e.g.,<br />
Al Shoot Irrig, Al Ain_Irrigated, Al Khazna Ag,<br />
etc.). The eastern-most porti<strong>on</strong> of the study<br />
domain includes a representati<strong>on</strong> of the Oman<br />
Mountain Wadis, and natural recharge to the<br />
shallow, freshwater aquifer (green square<br />
labeled Shallow E FR) occurs via a runoff link<br />
(blue dashed arrow) from Shwaib_Hayer_<br />
Swehan Irg object, leakage from the Swaib<br />
Dam object, which represents all surface water<br />
storage in Abu Dhabi, with a total capacity of 26<br />
mcm. This leakage rate was assumed as 20% of<br />
the previous m<strong>on</strong>th’s storage in the reservoir. It<br />
was assumed that <strong>on</strong>ly the East-Fresh aquifer<br />
is a renewable resource and undergoes modernday<br />
recharge via the Oman Mountains to the<br />
west of Al Ain.<br />
Other aquifers represented include those<br />
characterized by shallow brackish water<br />
(Shallow E BR), shallow saline (Shallow SA); and<br />
deeper sources such as East Aquitard Saline and<br />
Brackish. It was assumed that <strong>on</strong>ly the Shallow<br />
East-Fresh aquifer is a renewable resource and<br />
undergoes modern-day recharge via the Oman<br />
Mountains to the west of Al Ain. This recharge<br />
is represented by the Shwaib_Hayer_Sweihan<br />
Irg node, that in WEAP includes a natural, unirrigated<br />
land class which applies the same FAO<br />
Impacts, Vulnerability & Adaptati<strong>on</strong> for<br />
Water Resources in Abu Dhabi<br />
Table 4‐2. Municipal and industrial water demand, 2003.<br />
Populati<strong>on</strong><br />
Per capita demand (l/cap/day)<br />
Western 655,000 550<br />
Eastern 533,000 450<br />
105