Abstract
Shoreline hardening, which causes beach loss globally, will accelerate with sea level rise (SLR), causing more beach loss if management practices are not changed. To improve beach conservation efforts, current and future shoreline hardening patterns on sandy beaches need deeper analysis. A shoreline change model driven by incremental SLR (0.25, 0.46, 0.74 m) is used to simulate future changes in the position of an administrative hazard zone, as a proxy for risk of hardening at all sandy beaches on the island of O‘ahu, Hawai ‘i. In Hawai ‘i, hardening can be triggered when evidence of erosion is within 6.1 m (“20 ft”) of certain structures, allowing an applicant to request emergency protection. Results show an increase in shoreline vulnerability to hardening with SLR governed by backshore land use patterns. The largest increase (+ 7.6%) occurred between modern-day and 0.25 m of SLR (very likely by year 2050) with half of all beachfront shoreline at risk by 0.74 m of SLR. Maximum risk of shoreline hardening and beach loss is projected to occur from modern-day and near-term hardening because of the heavily developed aspect of some shoreline segments. Adaptation to SLR should be considered an immediate need—not solely a future issue.
Highlights
Shoreline hardening, which causes beach loss globally, will accelerate with sea level rise (SLR), causing more beach loss if management practices are not changed
Along other portions of the east side, overdevelopment and inappropriate road placement have led to considerable shoreline hardening and beach loss
Building on previous research of shoreline hardening patterns[18], this report analyzes the relationship of backshore land use and SLR on shoreline hardening
Summary
Shoreline hardening, which causes beach loss globally, will accelerate with sea level rise (SLR), causing more beach loss if management practices are not changed. Gittman et al.[18] compared hardening patterns to housing density, gross domestic product, coastal slope, accretion/erosion rates, geomorphology, mean tidal range, mean wave height, relative SLR, storm frequency, shoreline positions, and years since shoreline hardening was banned in that area for the coastline in the continental US. They offered future predictions of shoreline hardening development based on the understanding of the parameters described above. Oahu is used as a living laboratory of land use decisions, and, by extension, these results are indicative of beach conservation stresses in similar situations around the world
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