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climate change on UAE - Stockholm Environment Institute-US Center

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7 Vulnerability<br />

assessment of<br />

Drylands ecosystems<br />

This secti<strong>on</strong> will attempt to assess the<br />

vulnerability and impacts of drylands<br />

ecosystems with focus <strong>on</strong> Abu Dhabi emirates.<br />

It will present informati<strong>on</strong> <strong>on</strong> climatic <str<strong>on</strong>g>change</str<strong>on</strong>g>s,<br />

potential impacts and adaptati<strong>on</strong> measures for<br />

the drylands ecosystems.<br />

7.1. Observed Climatic <str<strong>on</strong>g>change</str<strong>on</strong>g>s in<br />

dryland ecosystems<br />

An assessment by the IPCC of l<strong>on</strong>g-term<br />

trends in precipitati<strong>on</strong> amount over many large<br />

regi<strong>on</strong>s for the period 1900-2005, indicated that<br />

drying has been observed in the Sahel, the<br />

Mediterranean, southern Africa and parts of<br />

southern Asia. The report has also indicated<br />

that more intense and l<strong>on</strong>ger droughts have<br />

been observed over wider areas since the 1970s,<br />

particularly in the tropics and subtropics (IPCC,<br />

2007). These observati<strong>on</strong>s are linked to higher<br />

temperatures, decreased precipitati<strong>on</strong>; <str<strong>on</strong>g>change</str<strong>on</strong>g>s<br />

in sea surface temperatures, wind patterns, and<br />

decreased snow cover.<br />

More relevant to dryland regi<strong>on</strong>s is that areas<br />

affected by drought have and will c<strong>on</strong>tinue to<br />

increase (IPCC, 2007). Little was reported in<br />

the IPCC Working Group 2 report regarding<br />

the observed impacts <strong>on</strong> crops and livestock in<br />

drylands or other developing country regi<strong>on</strong>s<br />

(Rosenzweig et al. 2007). A study had shown<br />

that very dry land areas across the globe<br />

(defined as areas with a PDSI of less than –3.0)<br />

have more than doubled in extent since the<br />

1970s, and this was associated with an initial<br />

precipitati<strong>on</strong> decrease over land related to<br />

the El Niño-Southern Oscillati<strong>on</strong> and with<br />

subsequent increases primarily due to surface<br />

warming (IIED, 2008).<br />

7.2 Projected climatic <str<strong>on</strong>g>change</str<strong>on</strong>g>s in<br />

dry land ecosystems<br />

The IPCC (2007) has left no doubt that global<br />

warming is occurring and that <str<strong>on</strong>g>climate</str<strong>on</strong>g> <str<strong>on</strong>g>change</str<strong>on</strong>g><br />

is human-induced, c<strong>on</strong>cluding that “warming of<br />

the <str<strong>on</strong>g>climate</str<strong>on</strong>g> system is unequivocal” and stating<br />

with 90 percent c<strong>on</strong>fidence that the net effect<br />

of human activities <strong>on</strong> Earth since 1750 has<br />

been warming. The report emphasized the high<br />

uncertainties in predicti<strong>on</strong> of arid ecosystem<br />

resp<strong>on</strong>ses to elevated CO 2 and global warming.<br />

However, it projected a generalized warming of<br />

over 3ºC and a 100% increase in frequency of<br />

extremely warm years and the likely reducti<strong>on</strong><br />

in rainfall in Southern Africa, Sahara & Central<br />

Asia and likely increase in West Africa, East<br />

Africa and South Asia (IPCC, 2007).<br />

7.3. Current <str<strong>on</strong>g>climate</str<strong>on</strong>g> and expected<br />

climatic <str<strong>on</strong>g>change</str<strong>on</strong>g> in the <strong>UAE</strong><br />

The <str<strong>on</strong>g>climate</str<strong>on</strong>g> of the <strong>UAE</strong> is characterized by high<br />

temperatures (up to 49ºC in July), high humidity<br />

and low rainfall. The average annual rainfall in<br />

the mountain regi<strong>on</strong> (140-200 mm) and al<strong>on</strong>g<br />

the east coast (100-140 mm) is generally higher<br />

compared to the gravel plains (100-120 mm),<br />

with the west coast receiving the lowest average<br />

of less than 60mm (Boer, 1997).<br />

The IPCC groups the Saudi peninsula into the<br />

Asian divisi<strong>on</strong>, a regi<strong>on</strong> expected to undergo a<br />

wide range of climatic <str<strong>on</strong>g>change</str<strong>on</strong>g>s over the next<br />

century. An assessment by the IPCC of trends in<br />

precipitati<strong>on</strong> for the period extending from 1900-<br />

2005 indicated that drying has been observed in<br />

the Sahel, the Mediterranean, southern Africa<br />

and parts of southern Asia, regi<strong>on</strong>s with similar<br />

<str<strong>on</strong>g>climate</str<strong>on</strong>g> characteristics to the peninsula. The<br />

IPCC reported that more intense and l<strong>on</strong>ger<br />

droughts have been observed over wider areas<br />

since the 1970s, particularly in the tropics and<br />

subtropics, but may have increased slightly in<br />

the Arabian Peninsula (IPCC, 2007).<br />

A recent c<strong>on</strong>sortium of <str<strong>on</strong>g>climate</str<strong>on</strong>g> scientists from<br />

the Middle East recently compiled a database<br />

of <str<strong>on</strong>g>climate</str<strong>on</strong>g> observati<strong>on</strong>s over the last half<br />

century, and reported that both maximum<br />

and minimum temperatures in the regi<strong>on</strong> have<br />

shown a statistically significant increase and the<br />

number days exceeding the 90 th percentile have<br />

increased throughout the regi<strong>on</strong> (Zhang et al.,<br />

2005). However, the report indicates that there<br />

have been no coherent trends in precipitati<strong>on</strong><br />

158<br />

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

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