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

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88 HURRICANES: THEIR NATURE AND IMPACf ON SOCIETY<br />

Midgets<br />

Ci) ~<br />

W<br />

(1935)<br />

LABOR DAY HURRICANE<br />

Normal to Large <str<strong>on</strong>g>Hurricanes</str<strong>on</strong>g><br />

tccc<br />

ANDREW (1992)<br />

Giant<br />

c<br />

~!~!)<br />

:::7<br />

NEW ENGLAND (1938)<br />

I I<br />

500km<br />

@)<br />

TRACY (1974)<br />

CAMILLE (1969)<br />

TIP (1979)<br />

GILBERT (1988)<br />

DIRECTION OF<br />

MOTION<br />

Figure 3.15 Relative size comparis<strong>on</strong> of the Labor Day Hurricane of 1935, the New<br />

Engl<str<strong>on</strong>g>and</str<strong>on</strong>g> Hurricane of 1938, Hurricane Camille (1969), Typho<strong>on</strong> Tracy (1974), Typho<strong>on</strong><br />

Tip (1979), Hurricane Gilbert, <str<strong>on</strong>g>and</str<strong>on</strong>g> Hurricane Andrew (1992). The approximate area<br />

with tropical storm shading is shown in light gray; the hurricane wind regi<strong>on</strong> is in black.<br />

The eye is shown by the white dot (adapted from Chip Guard (1997, pers<strong>on</strong>al<br />

communicati<strong>on</strong>) <str<strong>on</strong>g>and</str<strong>on</strong>g> McAdie <str<strong>on</strong>g>and</str<strong>on</strong>g> Rappaport (1991)). The storms are classified in this<br />

figure as midgets, normal to large, <str<strong>on</strong>g>and</str<strong>on</strong>g> giant. The informati<strong>on</strong> for the 1938 New<br />

Engl<str<strong>on</strong>g>and</str<strong>on</strong>g> hurricane was provided by E. Boose, 1997 (pers<strong>on</strong>al communicati<strong>on</strong>) using<br />

data from Boose, Foster <str<strong>on</strong>g>and</str<strong>on</strong>g> Fluet (1994). For the New Engl<str<strong>on</strong>g>and</str<strong>on</strong>g> Hurricane of 1938, the<br />

dashed line <strong>on</strong> the right side indicates that sustained tropical storm strength winds<br />

extended bey<strong>on</strong>d this distance. The informati<strong>on</strong> used to define the wind field for<br />

Hurricane Andrew in 1992 was obtained from Powell <str<strong>on</strong>g>and</str<strong>on</strong>g> Houst<strong>on</strong> (1996). Note that in<br />

the larger storms the area of hurricane winds is more uncertain, <str<strong>on</strong>g>and</str<strong>on</strong>g> thus is c<strong>on</strong>servatively<br />

underestimated in this figure

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