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Armoring on Eroding Coasts Leads to Beach Narrowing and Loss on Oahu, Hawaii

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Pitfalls of Shoreline Stabilization

Part of the book series: Coastal Research Library ((COASTALRL,volume 3))

Abstract

Coastal armoring (defined as any structure designed to prevent shoreline retreat that interacts with wave run-up at some point of the year) has, historically, been a typical response to managing the problem of beach erosion on the island of Oahu, Hawaii. By limiting the ability of an eroding shoreline to migrate landward, coastal armoring on Oahu has contributed to narrowing and complete loss of many kilometers of beach. In this paper, changes in beach width are analyzed along all armored and unarmored beaches on the island using historical shoreline positions mapped from orthorectified aerial photographs from as early as the late 1920s. Over the period of study, average beach width decreased by 11%±4% and nearly all (95%) documented beach loss was fronting armored coasts. Among armored beach sections, 72% of beaches are degraded, which includes 43% narrowed (28% significantly) and 29% (8.6km) completely lost to erosion. Beaches fronting coastal armoring narrowed by −36%±5% or −0.10±0.03m/year, on average. In comparison, beach widths along unarmored coasts were relatively stable with slightly more than half (53%) of beaches experiencing any form of degradation. East and south Oahu have the highest proportion of armored coast (35% and 39%, respectively) and experienced the greatest percent of complete beach loss (14% and 12%, respectively). West and north coasts, with relatively little armoring (10% and 12% armored, respectively), experienced little complete beach loss (2% and 6%, respectively). However, beaches are still significantly narrowed compared to historical patterns on west and north coasts (61% and 70%, respectively). We find at these sites that cultivation of coastal vegetation may be a factor in beach narrowing on Oahu, along with beach erosion. Increased ‘flanking’ erosion (accelerated shoreline retreat adjacent to armored sections) is documented at several beaches, often requiring extension of armoring structures to protect abutting coastal properties, a process that leads to alongshore seawall proliferation.

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Acknowledgments

This work was supported by grants from the State of Hawaii Department of Land and Natural Resources, City and County of Honolulu, Hawaii Sea Grant College Program, U.S. Army Corps of Engineers, Harold K.L. Castle Foundation, and Hawaii Coastal Zone Management Program. We thank Matthew Barbee, Chyn Lim, Tiffany Anderson, Haunani Kane, Matthew Dyer, Amanda Vinson, and Craig Sentor of the University of Hawaii Coastal Geology Group for their support on this project. Thank you to Neil Frazer of the University of Hawaii Geology and Geophysics Department for his advice on statistical methods. Thank you to Chris Conger and Dolan Eversole of Hawaii Sea Grant and Jessica Podoski of the U.S. Army Corps of Engineers for their advice on defining and mapping coastal armoring.

This paper is funded in part by a grant/cooperative agreement from the National Oceanic and Atmospheric Administration, Project R/IR-4, which is sponsored by the University of Hawaii Sea Grant College Program, SOEST, under Institutional Grant No. NA09OAR4170060 from NOAA Office of Sea Grant, Department of Commerce. The views expressed herein are those of the author(s) and do not necessarily reflect the views of NOAA or any of its subagencies. UNIHI-SEAGRANT-BC-09-02.

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Correspondence to Bradley M. Romine .

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Romine, B.M., Fletcher, C.H. (2012). Armoring on Eroding Coasts Leads to Beach Narrowing and Loss on Oahu, Hawaii. In: Cooper, J., Pilkey, O. (eds) Pitfalls of Shoreline Stabilization. Coastal Research Library, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-4123-2_10

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