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

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80<br />

CHAPTER 6<br />

FRESH WATER<br />

ences <strong>on</strong> the envir<strong>on</strong>ment, climate, ec<strong>on</strong>omy and<br />

culture <str<strong>on</strong>g>of</str<strong>on</strong>g> the coastal areas providing them with an<br />

important source <str<strong>on</strong>g>of</str<strong>on</strong>g> moisture and a heat reservoir.<br />

The situati<strong>on</strong> in the Mediterranean regi<strong>on</strong> is very<br />

complex due to large differences between different<br />

areas. While at its northwest coast populati<strong>on</strong><br />

growth has practically stopped, a two-fold<br />

increase is expected in North African countries<br />

during the first three decades <str<strong>on</strong>g>of</str<strong>on</strong>g> the 21 st century,<br />

with an even larger growth taking place in Syria<br />

and Palestine, adding more stress to the already<br />

scarce water resources. Global projecti<strong>on</strong>s present<br />

remarkable agreement <strong>on</strong> the Mediterranean<br />

regi<strong>on</strong>, where warming is expected to be larger<br />

than the global average with a large percent<br />

reducti<strong>on</strong> in precipitati<strong>on</strong> and an increase in<br />

inter-annual variability (Giorgi, 2006).<br />

Global simulati<strong>on</strong> can not be c<strong>on</strong>sidered accurate<br />

for the descripti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> the Mediterranean regi<strong>on</strong><br />

and downscaling by statistical methods and<br />

dynamic models can, in some situati<strong>on</strong>s, be used<br />

to provide better insight and give results with<br />

higher precisi<strong>on</strong>. Development <str<strong>on</strong>g>of</str<strong>on</strong>g> a regi<strong>on</strong>al<br />

model simulati<strong>on</strong> for the Mediterranean is<br />

presently missing and <strong>on</strong>e needs to be made in<br />

the future. Moreover, room should be left for different<br />

approaches such as statistical downscaling<br />

and other techniques.<br />

Leban<strong>on</strong>, taken as <strong>on</strong>e <str<strong>on</strong>g>of</str<strong>on</strong>g> the advanced countries<br />

with respect to climate change research, displays<br />

the following vulnerability issues (Assaf, 2009):<br />

• Chaotic urbanizati<strong>on</strong> at the expense <str<strong>on</strong>g>of</str<strong>on</strong>g> forests<br />

and wood lands.<br />

• Air, water and soil polluti<strong>on</strong>.<br />

• Increasing frequency <str<strong>on</strong>g>of</str<strong>on</strong>g> fires due to prol<strong>on</strong>ged<br />

dry seas<strong>on</strong>s.<br />

• <str<strong>on</strong>g>Change</str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> water table level due to excessive<br />

pumping and quarrying activities.<br />

• Overgrazing <str<strong>on</strong>g>of</str<strong>on</strong>g> rangelands.<br />

• Land fragmentati<strong>on</strong>.<br />

Morocco is another example <str<strong>on</strong>g>of</str<strong>on</strong>g> an <strong>Arab</strong><br />

Mediterranean country in which climate change<br />

research is well advanced. The country has prepared<br />

its First Nati<strong>on</strong>al Communicati<strong>on</strong> to the<br />

UNFCCC, and is in the process <str<strong>on</strong>g>of</str<strong>on</strong>g> developing<br />

the Sec<strong>on</strong>d Nati<strong>on</strong>al Communicati<strong>on</strong> Report.<br />

A map <str<strong>on</strong>g>of</str<strong>on</strong>g> composite indicators representing the<br />

vulnerability <str<strong>on</strong>g>of</str<strong>on</strong>g> both agriculture and domestic<br />

water uses to climate stress in the form <str<strong>on</strong>g>of</str<strong>on</strong>g> l<strong>on</strong>g<br />

hot and dry spells was generated to identify areas<br />

<str<strong>on</strong>g>of</str<strong>on</strong>g> high vulnerability. The results indicated that<br />

the ecosystem <str<strong>on</strong>g>of</str<strong>on</strong>g> the Tensift River Basin is very<br />

vulnerable with various degrees <str<strong>on</strong>g>of</str<strong>on</strong>g> vulnerability<br />

in different parts <str<strong>on</strong>g>of</str<strong>on</strong>g> the regi<strong>on</strong>.<br />

Libya has a prevailing Mediterranean climate<br />

and a geography characterized by coastal valleys<br />

and heights; rainy cold winters and dry hot summers;<br />

as well as the seas<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> spring and<br />

autumn in which the khamasin winds – locally<br />

called Gebli winds – blow. The country has ratified<br />

a number <str<strong>on</strong>g>of</str<strong>on</strong>g> United Nati<strong>on</strong>s agreements<br />

and protocols and is treated as <strong>on</strong>e <str<strong>on</strong>g>of</str<strong>on</strong>g> the Less<br />

Developed <strong>Countries</strong> in its mitigati<strong>on</strong> and<br />

adaptati<strong>on</strong> measures to climate change. Water<br />

resources in Libya are limited to rainfall in the<br />

north and modest quantities <str<strong>on</strong>g>of</str<strong>on</strong>g> groundwater in<br />

the south. C<strong>on</strong>tinued abstracti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> fossil<br />

groundwater will bring the country’s aquifers to<br />

a state <str<strong>on</strong>g>of</str<strong>on</strong>g> low feasibility by 2050.<br />

If the intensity <str<strong>on</strong>g>of</str<strong>on</strong>g> rainfall is reduced, as predicted<br />

by many sources, then the country will have<br />

no other opti<strong>on</strong> but to depend heavily <strong>on</strong> desalinati<strong>on</strong><br />

or to import surface water from neighbouring<br />

countries. Both alternatives are fairly<br />

costly especially as the country suffers a populati<strong>on</strong><br />

growth rate which ranges between 2.5 and<br />

3%.<br />

Syria is vulnerable to climate change because <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

the following reas<strong>on</strong>s:<br />

• More than 75% <str<strong>on</strong>g>of</str<strong>on</strong>g> the cropped area is dependant<br />

<strong>on</strong> rainfall as the main source <str<strong>on</strong>g>of</str<strong>on</strong>g> water.<br />

Therefore, fluctuati<strong>on</strong> in rainfall affects rainfed<br />

agriculture.<br />

• Fluctuati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> temperature affects crop yields.<br />

• Increased frequency and durati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> droughts<br />

affect crop producti<strong>on</strong> and food availability.<br />

In Egypt, rain-fed agriculture is limited to the<br />

north coast and is extended over a distance <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

1200 km where modest precipitati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> 100 –<br />

200 mm intensity falls every year, in particular<br />

during the winter m<strong>on</strong>ths (December -<br />

February). If this already limited amount <str<strong>on</strong>g>of</str<strong>on</strong>g> rain<br />

is reduced further, life in these regi<strong>on</strong>s will<br />

become intolerable unless Nile water is c<strong>on</strong>veyed<br />

from the east and west branches <str<strong>on</strong>g>of</str<strong>on</strong>g> the<br />

Damietta and Rosetta branches <str<strong>on</strong>g>of</str<strong>on</strong>g> the Nile.

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