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Impact of Climate Change on Arab Countries - (IPCC) - Working ...

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ARAB ENVIRONMENT: CLIMATE CHANGE 77<br />

• Nile Basin countries: Egypt and Sudan.<br />

• <strong>Arab</strong>ian Peninsula: Saudi <strong>Arab</strong>ia, Kuwait,<br />

United <strong>Arab</strong> Emirates, Qatar, Oman, Bahrain<br />

and Yemen.<br />

• Sahel countries: Somalia, Djipouti and<br />

Comoros Islands.<br />

Each <str<strong>on</strong>g>of</str<strong>on</strong>g> the above five regi<strong>on</strong>s has its distinct<br />

hydrological characteristics that can briefly be<br />

explained as follows:<br />

Al Mashrek Regi<strong>on</strong><br />

• Iraq and Syria are partially dependant <strong>on</strong> the<br />

Tigris and Euphrates rivers, originating from<br />

Turkey. The two countries have rainfall <str<strong>on</strong>g>of</str<strong>on</strong>g> reas<strong>on</strong>able<br />

intensity and groundwater potential in<br />

both countries is relatively high. Syria enjoys<br />

small flows caused by snow melt from the<br />

peaks <str<strong>on</strong>g>of</str<strong>on</strong>g> some local mountains.<br />

• Leban<strong>on</strong> depends <strong>on</strong> a number <str<strong>on</strong>g>of</str<strong>on</strong>g> local rivers<br />

or rivers shared with <strong>on</strong>e or more <str<strong>on</strong>g>of</str<strong>on</strong>g> the neighbouring<br />

countries.<br />

• The per capita shares <str<strong>on</strong>g>of</str<strong>on</strong>g> water in Leban<strong>on</strong> as<br />

well as in Syria and Iraq are the highest am<strong>on</strong>g<br />

all <strong>Arab</strong> countries.<br />

• Jordan and Palestine are the water poorest in<br />

this regi<strong>on</strong> since they depend up<strong>on</strong> the Jordan<br />

river and small quantities <str<strong>on</strong>g>of</str<strong>on</strong>g> rainfall and<br />

groundwater.<br />

Al Maghreb Regi<strong>on</strong><br />

• All five Maghreb countries depend mainly <strong>on</strong><br />

rainfall and partially <strong>on</strong> modest groundwater<br />

reserves.<br />

Nile Basin Regi<strong>on</strong><br />

• The southern part <str<strong>on</strong>g>of</str<strong>on</strong>g> Sudan enjoys ample precipitati<strong>on</strong><br />

which can meet the prevailing evaporative<br />

demand; however, rain gradually vanishes<br />

north <str<strong>on</strong>g>of</str<strong>on</strong>g> the capital Khartoum. Following<br />

the signing <str<strong>on</strong>g>of</str<strong>on</strong>g> the Nile Water Agreement in<br />

1959, Sudan and Egypt divided the average<br />

natural flow at Aswan (84 billi<strong>on</strong> m 3 /year) to<br />

<strong>on</strong>e quarter for Sudan (18.5 billi<strong>on</strong> m 3 /year),<br />

three quarters for Egypt (55.5 billi<strong>on</strong> m 3 /year)<br />

and the remaining 10 billi<strong>on</strong> m 3 /year were left<br />

to make up for natural evaporati<strong>on</strong> from Lake<br />

Nasser.

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