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climate change on UAE - Stockholm Environment Institute-US Center

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water to meet its demands, Unmet Demand for<br />

this sector can be thought of as “additi<strong>on</strong>al<br />

desalinizati<strong>on</strong> capacity needed”. For the<br />

forestry and agriculture sector that rely <strong>on</strong><br />

groundwater, “unmet demand” suggests the<br />

n<strong>on</strong>-sustainability of the water use activity and/<br />

or the overdrafting of groundwater aquifers.<br />

For the analysis of water supply, we will focus<br />

<strong>on</strong> the Optimistic with Adaptati<strong>on</strong> (1.1) and<br />

the Pessimistic with Adaptati<strong>on</strong> (2.1), where<br />

both include their respective <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g><br />

forcing. From this analysis, it is very apparent<br />

that unless future per-capita water use is not<br />

substantially curtailed, future demands will<br />

<strong>on</strong>ly be met through increased desalinizati<strong>on</strong><br />

capacity, while the agriculture and forestry<br />

sectors would increasingly need to turn to<br />

more saline groundwater to meet irrigati<strong>on</strong><br />

requirements. Renewable freshwater resources<br />

in the eastern porti<strong>on</strong> of the ADE are simply<br />

not substantial enough to be c<strong>on</strong>sidered a<br />

major c<strong>on</strong>tributor to the future water resource<br />

portfolio <strong>on</strong> the ADE.<br />

In Figure 5-3, desalinzed water supply grows<br />

up to its currently installed capacity but then<br />

capacity does not <str<strong>on</strong>g>change</str<strong>on</strong>g> over study horiz<strong>on</strong>.<br />

Fresh groundwater resources remain c<strong>on</strong>stant.<br />

To c<strong>on</strong>tinue to support irrigated agriculture<br />

where brackish groundwater sources are<br />

inadequate, irrigati<strong>on</strong> requirements are madeup<br />

through pumping of saline groundwater<br />

supplies. Fresh groundwater supplies remain<br />

nearly c<strong>on</strong>stant, as they have been c<strong>on</strong>strained<br />

to make up <strong>on</strong>ly 10% of the total groundwater<br />

supply in WEAP, otherwise the alluvial,<br />

freshwater aquifers in the western porti<strong>on</strong> of<br />

the ADE would be quickly overdrafted. Once<br />

this 10% of demand is met through the fresh<br />

groundwater resource, brackish and then saline<br />

groundwater sources can supply the remaining<br />

irrigati<strong>on</strong> needs.<br />

WEAP assumes that all sources can adequately<br />

supply crop water requirements, as WEAP<br />

makes no distincti<strong>on</strong> between water supply type,<br />

except the distincti<strong>on</strong> of preference from which<br />

supply to draw from first (e.g. first brackish<br />

and if there is an inadequate supply, then draw<br />

from the saline groundwater). The supply<br />

allocati<strong>on</strong> for the Pessimistic with Adaptati<strong>on</strong><br />

(2.1) Scenario is nearly identical to Scenario 1.1<br />

because we have c<strong>on</strong>strained supply to current<br />

levels (e.g. no <str<strong>on</strong>g>change</str<strong>on</strong>g> in desalinized water or<br />

waste water treatment expansi<strong>on</strong>).<br />

Figure 5.4 shows the estimated unmet demands<br />

Total Unmet Demand<br />

Figure ‎5‐4. Total unmet demand for the Optimistic and Pessimistic Scenarios with Adaptati<strong>on</strong>.<br />

120<br />

Climate Change Impacts, Vulnerability & Adaptati<strong>on</strong>

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