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Coastal Subsidence Study 2005
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Coastal Subsidence Study 2005
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Using another method such as a set datum, elevation or topography to <br />determine the shoreline is ruled out in this study because it would require extensive <br />changes at the statutory and regulatory level. Also, on-going subsidence would make <br />the use of a set datum or elevation outdated after many years. Another difficulty <br />would be the significant topography changes within the same property. <br /> The case can be made that the shoreline at Kapoho should not be determined <br />by high tide events, but high wave events. Under the current shoreline definition, this <br />would exclude storm and seismic (tsunami) events but not seasonal high surf from <br />distant swells. Actually, under the definition both high tide and wave run-up should <br />be considered. It was outside the scope of this study, but it is generally felt that high <br />tide events are most useful for Kapoho area because wave runup is limited by wave <br />height which is limited by the depth of water over Waiopae Road. Supposedly, <br />further studies could have been conducted that made a comparison of high tide events <br />with lesser tides coinciding with high non-storm surf. This was outside the scope of <br />the study. Furthermore, the need to even do this illustrates some of the problems with <br />the shoreline certification process. A thesis or dissertation should not be needed to <br />determine the shoreline, because it only determines the baseline from which other <br />15 <br />regulatory or development standards apply (e.g., the setback). <br /> 3.4.6 Waiver <br /> The Hawaii County Department of Planning could also use their power of <br />waiver, under their SMA rules. Under Section 9-10(B)(9) – A shoreline survey (is <br />required) when the parcel abuts the shoreline, except that the Director may waive the <br />submission of the survey when the proposed development is clearly and unmistakably <br />located on a shoreline parcel at a considerable distance from the shoreline. It could <br />be argued that the areas mauka of Waiopae Road subject to flooding by gravity flow <br />are a considerable distance from the shoreline. Also under the Hawaii County <br />shoreline setback rules, Section 11-4(c) the Planning Department may waive the <br />certification requirement in cases in which there may be unusual physical <br />circumstances or conditions of the land. The case can be made that these <br />circumstances apply to Kapoho given the subsidence, natural topography and existing <br />development. <br /> Perhaps the waiver would be acceptable if the shoreline was occasionally <br />flooding but stable. However, the problem of using the waiver in the Kapoho area is <br />that if an area is flooding, it is likely to get worse from ongoing subsidence. It may be <br />possible to resolve this issue by considering the level of flooding and projecting <br />future flooding problems by using a rate of subsidence and the slope of the land. <br />15 <br /> In the 1994 report on Shoreline Certification Review and Recommendations, it was recommended that <br />the shoreline be interpreted in a way that is simple to identify and administrate. Thus increased emphasis <br />on the vegetation line was proposed. Fletcher and Hwang – 1994. <br />37 <br /> <br />
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