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Flood Risk and Vulnerability Analysis Project - Atlantic Climate ...

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Storms weaken rapidly once they make l<strong>and</strong>fall <strong>and</strong> most such storms have not been of<br />

Hurricane force when hitting Newfoundl<strong>and</strong>, especially western Newfoundl<strong>and</strong> given that<br />

for a hurricane to pass west of the isl<strong>and</strong>, it would almost necessarily have had to pass<br />

over some part of the Maritimes <strong>and</strong> would have been weakened considerably as a<br />

result;<br />

Several peer-reviewed studies show a global trend toward increased intensity of the<br />

strongest hurricanes over the past several decades. The strongest trends are in the<br />

North <strong>Atlantic</strong> Ocean <strong>and</strong> the Indian Ocean. This is consistent with this study‟s findings.<br />

Figure 3-17 confirms the increase in the last several decades. Figure 3-18 also shows<br />

an increase in Tropical Storms entering Newfoundl<strong>and</strong> coastal waters in the last 2<br />

decades <strong>and</strong> a very marked increase of storms making l<strong>and</strong>fall in eastern Newfoundl<strong>and</strong><br />

in the last decade. According to the 2007 Fourth Assessment Report of the<br />

Intergovernmental Panel on <strong>Climate</strong> Change (IPCC-AR4), it is “more likely than not”<br />

(better than even odds) that there is a human contribution to the observed trend of<br />

hurricane intensification since the 1970s. In the future, “it is likely [better than 2 to 1<br />

odds] that future tropical cyclones (typhoons <strong>and</strong> hurricanes) will become more intense,<br />

with larger peak wind speeds <strong>and</strong> more heavy precipitation associated with ongoing<br />

increases of tropical sea surface temperatures”;<br />

Bruce (2011) also points out that with increasing global temperatures <strong>and</strong> increasing<br />

equatorial water temperatures, more intense Hurricanes are likely to develop <strong>and</strong>, while<br />

tracks are not expected to change, the storms will retain greater force as they reach<br />

more northern latitudes. While it is not possible to state that any particular event is or is<br />

not a result of global warming, Hurricane Igor, was able to retain Category 1 strength as<br />

it passed over the Avalon Peninsula (see track at Figure 3-27) <strong>and</strong> it caused the most<br />

devastating floods in Newfoundl<strong>and</strong> history (see Figure 2-2).<br />

Hurricanes <strong>and</strong> Tropical Storms combine intense rainfall with very strong winds<br />

(Category 1 Hurricanes ≥ 120 km/hr) producing significant storm surge <strong>and</strong> wind induced<br />

waves;<br />

Though there will likely continue to be decades in the future with greater <strong>and</strong> lesser<br />

activity, more intense Hurricanes <strong>and</strong> Tropical Storms will likely affect the isl<strong>and</strong> of<br />

Newfoundl<strong>and</strong> with the higher intensity storms impacting especially the Eastern WRMD<br />

many of whose coastal communities would also be subject to storm surge <strong>and</strong> waves;<br />

In terms of worst case scenario for these cyclones, consider the Saxby Gale of Oct<br />

1869:<br />

o<br />

This „gale‟ was essentially a Hurricane which tracked over Cape Cod <strong>and</strong> made<br />

l<strong>and</strong>fall in Maine, <strong>and</strong> then tracked across northern New Brunswick ( see Figure<br />

3-27);<br />

TA1112733 page 83

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