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Hurricanes: Their Nature and Impacts on Society - Climate Science ...

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78<br />

HURRICANES: THEIR NATURE AND IMPACT ON SOCffiTY<br />

Figure 3.9 A model simulati<strong>on</strong> of the eye <str<strong>on</strong>g>and</str<strong>on</strong>g> eye wall regi<strong>on</strong> of a mature hurricane.<br />

The c<strong>on</strong>tours show wind speed in miles per hour. The solid c<strong>on</strong>tours represent winds<br />

moving into the page <str<strong>on</strong>g>and</str<strong>on</strong>g> dashed c<strong>on</strong>tours represent winds moving out of the page. The<br />

shaded regi<strong>on</strong> illustrates the locati<strong>on</strong>s of cloud. Figure provided by Dr Mel Nicholls,<br />

Colorado State University; this work is also reported in Nicholls <str<strong>on</strong>g>and</str<strong>on</strong>g> Pielke (1995)<br />

l<str<strong>on</strong>g>and</str<strong>on</strong>g>fall because of the wann water of the Gulf Stream (Willoughby <str<strong>on</strong>g>and</str<strong>on</strong>g> Black<br />

1996).*<br />

Fortunately, few hurricanes attain their theoretical maximum potential<br />

intensity. The presence of significant vertical wind shear is likely the major<br />

reas<strong>on</strong> that hurricanes do not attain this level of intensity.<br />

* There are several theories <strong>on</strong> the maximum potential intensity of tropical cycl<strong>on</strong>es (Gray<br />

1997). The heat engine analog of these storms has been used to estimate maximum possible<br />

strength based <strong>on</strong> inflow <str<strong>on</strong>g>and</str<strong>on</strong>g> outflow temperature differences (Emanuel 1986; 1987). Emanuel et<br />

al. (1995) use this c<strong>on</strong>cept to propose that extremely str<strong>on</strong>g hurricanes could develop, which they<br />

call "hypercanes". A different mechanism has also been proposed where hurricane intensity is<br />

limited by c<strong>on</strong>trols <strong>on</strong> deep cumulus cloud buoyancy in the eye wall (Holl<str<strong>on</strong>g>and</str<strong>on</strong>g> 1997). William<br />

Gray of Colorado State University, however, maintains that upper-level momentum export from<br />

the storm, al<strong>on</strong>g with surface fricti<strong>on</strong>al dissipati<strong>on</strong> must be c<strong>on</strong>sidered together with the thermodynamic<br />

c<strong>on</strong>trols proposed by Emanuel <str<strong>on</strong>g>and</str<strong>on</strong>g> by Holl<str<strong>on</strong>g>and</str<strong>on</strong>g> (Gray 1997).

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