Coastal Construction Manual - National Ready Mixed Concrete ...
Coastal Construction Manual - National Ready Mixed Concrete ...
Coastal Construction Manual - National Ready Mixed Concrete ...
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3 IDENTIFYING HAZARDS<br />
TERMINOLOGY<br />
WAVE RUNUP is the rush of water up a slope or structure.<br />
WAVE RUNUP DEPTH at any point is equal to the maximum wave runup elevation minus the lowest<br />
eroded ground elevation at that point.<br />
WAVE RUNUP ELEVATION is the elevation reached by wave runup, referenced to NGVD or other<br />
datum.<br />
WAVE SETUP is an increase in the stillwater surface elevation near the shoreline, due to the presence<br />
of breaking waves. Wave setup typically adds 1.5 to 2.5 feet to the 100-year stillwater flood elevation.<br />
MEAN WATER ELEVATION is the sum of the stillwater elevation and wave setup.<br />
3.6.7 Erosion Considerations and Flood Hazard Mapping<br />
Proper design requires two types of erosion to be considered: dune and bluff erosion during the base flood<br />
event, and long-term erosion. Newer FIRMs account for the former, but no FIRMs account for the latter.<br />
Dune/Bluff Erosion. Current FIS procedures account for the potential loss of protective dunes and bluffs<br />
during the 100-year flood. However, this factor was not considered in coastal FIRMs prepared prior to May<br />
1988, which delineated Zone V without any consideration for storm-induced erosion. Zone V boundaries<br />
were drawn at the crest of the dune solely on the basis of the elevation of the ground and without regard for<br />
the erosion that would occur during a storm.<br />
Long-Term Erosion. Designers, property owners, and floodplain managers should be careful not to assume<br />
that flood hazard zones shown on FIRMs accurately reflect current flood hazards, especially if there has<br />
been a significant natural hazard event since the FIRM was published. For example, flood hazard restudies<br />
completed after Hurricane Opal (1995, Florida Panhandle) and Fran (1996, Topsail Island, NC) have<br />
produced FIRMs that are dramatically different from the FIRMs in effect prior to the hurricanes.<br />
Figure 3-57 provides an example of the effects of both dune erosion and long-term erosion changes. The figure<br />
compares pre- and post-storm FIRMs for Surf City, NC. The map changes are attributable to two factors:<br />
(1) pre-storm FIRMs did not show the effects of erosion that occurred after the FIRMs were published and<br />
did not meet technical standards currently in place, and (2) Hurricane Fran caused significant changes to the<br />
topography of the barrier island. Not all coastal FIRMs would be expected to undergo such drastic revisions<br />
after a flood restudy; however, many FIRMs may be in need of updating, and designers should be aware that<br />
FIRMs may not accurately reflect present flood hazards at a site.<br />
3.6.8 Dune Erosion Procedures<br />
Current Zone V mapping procedures (FEMA 2003) require that a dune have a minimum frontal dune<br />
reservoir (dune cross-section above 100-year stillwater level and seaward of dune peak) of 540 square feet<br />
in order to be considered substantial enough to withstand erosion during a base flood event. According<br />
to FEMA procedures, a frontal dune reservoir less than 540 square feet will result in dune removal (dune<br />
disintegration), while a frontal dune reservoir greater than or equal to 540 square feet generally will result in<br />
dune retreat (see Figure 3-58).<br />
3-62 COASTAL CONSTRUCTION MANUAL