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

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a near certainty, <strong>and</strong> an occurrence before 2050 (for a Category 2) <strong>and</strong> before 2080 (for<br />

Category 3) cannot be ruled out;<br />

A hurricane making l<strong>and</strong>fall on the isl<strong>and</strong> would produce the very highest water levels in<br />

Newfoundl<strong>and</strong>. A very coarse preliminary attempt at quantifying the cumulative factors<br />

was presented for illustration purposes only. Numerous other factors unique to each<br />

storm <strong>and</strong> its behavior as well as the local topography would affect that high water mark<br />

both downward as well as upward; <strong>and</strong><br />

As a result, it is recommended that other opinions be obtained, that further studies be<br />

commissioned to more precisely estimate the high water levels, <strong>and</strong> that appropriate<br />

emergency plans be developed.<br />

3.4.8 Recommendations for Assessment of <strong>Climate</strong> Change Impacts<br />

The following general recommendations are offered to assist the Government of Newfoundl<strong>and</strong><br />

<strong>and</strong> Labrador in designing <strong>and</strong> implementing future studies that involve climate change analysis.<br />

1. It is recommended that WRMD develop updated <strong>and</strong> projected IDF relationships for<br />

locations across the Province with suitable past precipitation intensity records. While<br />

IDFs characterize only one flood risk factor, precipitation, <strong>and</strong> do not capture the<br />

seasonality of precipitation, developing projected IDFs for future time frames is a<br />

worthwhile exercise especially if a means can be found to incorporate in that effort, the<br />

results of dynamical modeling of hurricanes to 2050 <strong>and</strong> beyond. Seasonal IDFs could<br />

also be developed <strong>and</strong> may be useful given that specific hazards are associated with<br />

particular seasons (e.g., hurricanes/tropical storms in the fall <strong>and</strong> Weather Bombs in the<br />

fall <strong>and</strong> early winter).<br />

2. It is recommended that WRMD require that future net sea level rise be incorporated into<br />

flood plain map development for coastal communities.<br />

3. It is recommended that the Province of NL actively track ocean-atmosphere oscillations<br />

in an effort to predict climate anomalies <strong>and</strong> hurricane intensity in particular years or<br />

series of years in the future. The warm <strong>and</strong> cold cycles in the various ocean-atmosphere<br />

oscillations that influence tropical storm frequency <strong>and</strong> intensity <strong>and</strong> other aspects of<br />

Newfoundl<strong>and</strong> <strong>and</strong> Labrador weather year-over-year, will also continue through to the<br />

end of this century though their periodicity <strong>and</strong> intensity may change over the coming<br />

decades.<br />

4. It is recommended that the Province of NL complete a more detailed analysis of Weather<br />

Bombs, similar to that conducted within this study on Tropical Systems, to determine if<br />

these storms, often approaching Hurricane strength, are increasing in intensity <strong>and</strong>/or<br />

frequency. This would be particularly useful in assessment flood potential on the isl<strong>and</strong><br />

of Newfoundl<strong>and</strong>‟s east <strong>and</strong> north coasts.<br />

TA1112733 page 92

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