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

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Worst Case Scenarios<br />

This section provided a preliminary assessment of weather phenomena or combinations<br />

of weather events <strong>and</strong> other circumstances which, when occurring simultaneously or in<br />

succession, can lead to significant flooding. While somewhat rare (an occurrence every<br />

few years or less often), most of the scenarios have occurred in the past <strong>and</strong> are likely to<br />

occur again, <strong>and</strong> so this section does not deal, per se, with highly unlikely events but<br />

rather very plausible events (one could conjure up much worst case scenarios);<br />

<br />

<br />

<br />

<br />

Considering, from the modeling work done here <strong>and</strong> reported elsewhere, the more<br />

marked increases in temperature <strong>and</strong> precipitation in the winter season <strong>and</strong> supported<br />

somewhat by updated IDFs, it is likely that winter rains will occur more frequently in the<br />

coming decades which gives rise to a number of scenarios all starting with abundant<br />

winter rains:<br />

o<br />

o<br />

o<br />

Combined with sudden melting of the winter snow pack to produce a greater threat of<br />

flooding especially likely for the West WRMD;<br />

Together with sudden prolonged warming sufficient to break up river ice causing ice<br />

jams as has happened at Badger in 2003, Central WRMD;<br />

Falling on frozen ground unable to absorb the added moisture which did lead to a<br />

major flood in Ontario in 1980 (noted again that Newfoundl<strong>and</strong> may be especially<br />

vulnerable given the thin soils);<br />

Weather Bombs are explosively deepening low pressure systems typically starting in the<br />

Cape Cod area <strong>and</strong> tracking just east of Newfoundl<strong>and</strong> as they continue to intensify<br />

rapidly. Such storms produce very strong (sometimes over 100 km/hr) wind b<strong>and</strong>s<br />

which can generate, thanks to a fetch of many hundreds of kilometers across the North<br />

<strong>Atlantic</strong>, very significant waves. These are the „Nor‟easters‟ for which Newfoundl<strong>and</strong> is<br />

famous. They are a threat especially for the coastal communities on the eastern <strong>and</strong><br />

northern sides of the isl<strong>and</strong> of Newfoundl<strong>and</strong> <strong>and</strong> it is speculated that they could<br />

increase in intensity, but likely not in frequency, under a warming climate scenario.<br />

Weather Bombs warrant closer examination, not possible here, given that they can<br />

approach Hurricane intensity.<br />

Hurricanes <strong>and</strong> tropical storms present the greatest threat of producing severe flooding<br />

for Newfoundl<strong>and</strong>. The intensity <strong>and</strong> frequency of tropical systems affecting<br />

Newfoundl<strong>and</strong> <strong>and</strong> neighboring waters has increased in the last several decades <strong>and</strong><br />

especially since 2000. Hurricane level storms, Category 1 <strong>and</strong> 2, have occurred but<br />

remain rare events <strong>and</strong> so it is not possible to give precise return periods for these<br />

especially given the cyclical nature of some of the oscillations that may influence them;<br />

Many references support the argument that warmer tropical oceans together with<br />

warmer waters in the North <strong>Atlantic</strong> will allow more tropical systems to maintain greater<br />

intensity as they track northward along the east coast of North America. As such, it can<br />

be said that a Category 2 or 3 hurricane making l<strong>and</strong>fall in Newfoundl<strong>and</strong> is likely, if not<br />

TA1112733 page 91

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