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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a sec<strong>on</strong>d landfall in the Islamic Republic of Iran.<br />
While historical record does not go back very far,<br />
these types of storms are very, very unusual for<br />
this part of the world. G<strong>on</strong>u, and the possibility<br />
of a similar storm in the future, raised c<strong>on</strong>cern<br />
due to the Gulf regi<strong>on</strong>’s s sensitive coastal<br />
infrastructure of heavy oil drilling activities,<br />
tanker traffic, and coastal populati<strong>on</strong> density.<br />
As a sizeable porti<strong>on</strong> of the world’s petroleum<br />
exports go through the Gulf of Oman, any<br />
slight blip in supply or exporting could be quite<br />
noticeable <strong>on</strong> the world markets.<br />
Figure 2‐9. Tropical Cycl<strong>on</strong>e G<strong>on</strong>u churns off the<br />
coast of the Middle East and southern Asia (NASA).<br />
In 2007, Cycl<strong>on</strong>e G<strong>on</strong>u became the first<br />
documented Category-5 cycl<strong>on</strong>e in the<br />
Arabian Sea. G<strong>on</strong>u made landfall in Oman<br />
with maximum sustained winds near 148 km/<br />
hr. In Oman, the cycl<strong>on</strong>e affected more than<br />
20,000 people and was resp<strong>on</strong>sible for more<br />
than 50 fatalities. In Figure 2‐9, Cyl<strong>on</strong>e G<strong>on</strong>u<br />
approaches the Gulf of Oman and Strait of<br />
Hormuz (NASA, n.d.).<br />
G<strong>on</strong>u moved through the Arabian Gulf making<br />
Some recent global <str<strong>on</strong>g>climate</str<strong>on</strong>g> model experiments<br />
suggest a future decline in tropical cycl<strong>on</strong>e<br />
frequency (Royer et al., 1998) while others argue<br />
for an increased likelihood of <str<strong>on</strong>g>change</str<strong>on</strong>g>s in the<br />
tropical storms in the event of global warming<br />
(Knuts<strong>on</strong> et al., 1999; Henders<strong>on</strong>-Sellers et<br />
al., 1998; Royer et al., 1998 and Krishnamurti<br />
et al., 1998; Elsner et al., 2008). Although the<br />
studies carried out so far are inc<strong>on</strong>clusive <strong>on</strong><br />
the likely <str<strong>on</strong>g>change</str<strong>on</strong>g>s in frequency of cycl<strong>on</strong>es,<br />
it is almost certain that an increase in sea<br />
surface temperature will be accompanied by<br />
a corresp<strong>on</strong>ding increase in cycl<strong>on</strong>e intensity.<br />
Recent studies suggest a possible increase<br />
in cycl<strong>on</strong>e intensity of 10-20% for a rise in sea<br />
Figure 2‐10. Area of str<strong>on</strong>ger than normal northwesterly winds (Shamal) and higher wind waves.<br />
24<br />
Climate Change Impacts, Vulnerability & Adaptati<strong>on</strong>