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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>

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