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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

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