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Chapter 10:Hazard Analysis—Floods <br /> controlled to meet FEMA mapping standards. These data were assimilated together with the <br /> best available bathymetric datasets, including USACE hydrographic LiDAR, into high- <br /> resolution seamless digital elevation models. <br /> The hazard analysis considered the combination of storm surge and hurricane-induced wave <br /> hazards. This included independent analysis and/or modeling of storm surge, return <br /> frequency flood elevations, wave setup, overland wave hazards, and wave runup. The <br /> ADvanced CIRCulation model for coastal ocean hydrodynamics (ADCIRC) was selected to <br /> develop the stillwater elevations or storm surge for the study area. The Empirical Simulation <br /> Technique (EST), also developed by the USACE, was used to determine the stillwater <br /> frequency curves for the 10-, 2-, 1-, and 0.2-percent annual chance stillwater elevations. <br /> Deepwater wave conditions were determined using the Shore Protection Manual (SPM) <br /> prediction technique and limited fetch analyses were performed in harbor and sheltered areas. <br /> Wave setup was differentiated and evaluated for areas with and without fronting reefs. Areas <br /> of primary frontal dune were identified, delineated, and eroded. Overland wave propagation <br /> hazards were evaluated using the WHAFIS model. Wave obstructions were verified at <br /> representative transect locations by field reconnaissance. Wave run-up was evaluated using <br /> the RUNUP 2.0 and TAW methodologies, depending of the presence of reefs and local <br /> steepness of the bathymetry. <br /> Wave hazard analyses were conducted at FIS transect locations, in addition to more tightly- <br /> spaced"mapping transacts." These additional transacts were facilitated by the application of <br /> an integrated GIS toolset that automates repetitive modeling tasks, and enables a more <br /> detailed analysis than typical coastal FIS studies. Wave setup values were assigned to these <br /> transects according to analysis at adjacent FTS transects. Otherwise, the mapping transects <br /> were treated with the same overland wave propagation and wave runup assessments as the <br /> FIS transects. <br /> The coastal hazards determined from the above analyses were synthesized in the form of the <br /> standard FEMA special flood hazard boundaries for the Zone VE, Zone AE, Zone AO, and <br /> Zone X hazard areas. These are presented in the TSDN as workmaps produced at a scale of <br /> 1':500". The workmaps also include stillwater stations, topographic elevation contours, FIS <br /> and mapping transect locations, and the shoreline. Wave analysis for the 0.2%annual chance <br /> event was not included in the scope of the study. The 0.2% return frequency stillwater <br /> elevation was exceeded by cumulative flood elevation from the 1% stillwater elevation and <br /> wave setup, therefore, the boundary of the 0.2% annual chance event was not delineated. To <br /> steeper areas where mapping scale limits the gutter placement, the SFHAs are only identified <br /> by the position of the 100-yr flood boundary. Mapped Base Flood Elevations (BFEs) are <br /> considerably dependent to the topographic representation at each transect. As a result, <br /> localized variations in the topography at other locations may not be fully reflected in the <br /> mapped SFHAs and BFEs. <br /> A Technical Support Data Notebook (TSDN) was compiled for each county in the study <br /> area. Storm surge and return frequency elevation analyses were inclusive of all counties, and <br /> thus all materials pertaining to those analyses, including model input, output, and <br /> documentation are included in each county TSDN. The remainder of the data, including <br /> wave modeling, mapping, workmaps, topography, etc., are island and county specific. <br /> Therefore,these data are only presented in the appropriate countywide TSDN. <br /> 10-34 Hawaii County Multi-Hazard Mitigation Plan <br />