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Potomac Waterfront Flood Mitigation Study - City of Alexandria

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Table 4-1: Repetitive Loss Properties within <strong>Study</strong> Area<br />

Address Notes FFE (NAVD88)<br />

110 Cameron St<br />

Condos #110, 102, 103, &<br />

104<br />

4.6<br />

1 King St. Boat Club 3.75<br />

6 King St Mai Thai 3.5<br />

101 King St<br />

Same building as 103 King<br />

St<br />

5.0<br />

104 S. Union St -- 3.9<br />

Technical Analyses Support<br />

It should be noted that the FFE listed in the <strong>City</strong>’s repetitive loss database for 110 Cameron<br />

Street appears to be unfinished storage space for all units. Based on our field review, the FFE is<br />

above the extreme flood level. However, since this property has been identified as a repetitive<br />

loss structure by FEMA, flood mitigation measures were identified for this structure.<br />

Section 6 lists flood protection provided for the repetitive loss properties for each structural<br />

mitigation measure. All <strong>of</strong> these properties have a recommended mitigation alternative. This<br />

recommendation may not protect the property from every flood event; however, it will reduce<br />

the frequency <strong>of</strong> flood damages. A reduction in flood damages directly reduces the impact to the<br />

property owner, and the amount <strong>of</strong> time the <strong>City</strong> spends supporting that property owner. In<br />

addition, a reduction in the frequency <strong>of</strong> flood damage is considered by FEMA to be successful<br />

mitigation for a repetitive loss property, thus improving the <strong>City</strong>’s CRS score.<br />

4.5 CONSIDERATION OF SEA LEVEL RISE<br />

Because flood control structures proposed in this study have design lifetimes greater than 10<br />

years, the potential effects <strong>of</strong> climate change on the <strong>Potomac</strong> River were considered. Climate<br />

change is a subtle, yet progressive change in climatic conditions such as temperature and<br />

precipitation over a given period <strong>of</strong> time. Climate data records illustrate a significant climate<br />

shift in the early 1900s, and further studies indicate that climate change is occurring ever more<br />

rapidly, although changes differ regionally and seasonally. Climate change occurs from natural<br />

climatic variations, teleconnections (correlation between oceanic and atmospheric anomalies),<br />

and human activity. Confirmation <strong>of</strong> a global temperature rise comes from the observed<br />

temperature increases in the oceans, observations <strong>of</strong> sea level rise, and diminished snow cover in<br />

the Northern Hemisphere.<br />

A small temperature increase (say 2 o Centigrade [C]), expected by the end <strong>of</strong> the 21 st century,<br />

will drastically impact human life and the future global economy and environment. Global<br />

warming alters the hydrologic balance, resulting in extreme events such as drought and heat,<br />

increase in the power <strong>of</strong> hurricanes, decreased water flow in rivers, melting <strong>of</strong> glaciers, and<br />

increased variability in precipitation and flood risks.<br />

<strong>Flood</strong>ing Issues<br />

Climate change results in increased precipitation intensity and variability, which change the<br />

antecedent conditions <strong>of</strong> river basins and river flows. Higher intensity precipitation events will<br />

significantly increase flood risks. Moreover, rising sea levels will increase flood risks in tidally<br />

28-JUL-10\\ 4-8

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