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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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>