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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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>