Details:

Journal Title:
Coastal Engineering
Personal Author:
Ludka, B.C. ; Guza, R.T. ; O'Reilly, W.C.
Ludka, B.C. ; Guza, R.T. ; O'Reilly, W.C. Less -
NOAA Program & Office:
OAR (Oceanic and Atmospheric Research) ; Sea Grant
OAR (Oceanic and Atmospheric Research) ; Sea Grant Less -
Sea Grant Program:
CASG/CUIMR (California Sea Grant)
Description:
Four southern California beaches were nourished with offshore sand placed as subaerial pads several meters thick, 50 m wide, and spanning between 500 and 1500 m alongshore. Three nourishments constructed with coarser than native sand, placed in 2012 at Imperial, Cardiff and Solana Beaches, elevated subaerial sand volumes for several years even when exposed to the energetic winter waves of the 2015-16 El Niño, followed by a stormy 2016-17 winter. As these relatively resilient pads were overwashed, landward tilted subaerial profiles (accretionary crowns) formed at the eroding front face of the originally flat-topped pads and pooling occurred in the backbeach. At Imperial Beach, nourishment sand helped prevent waves from directly impacting riprap fronting houses, while groundwater flooding behind the pad was observed at a location where the pad was elevated 1.6 m above the street. As the nourishments retreated, alongshore oriented spits grew downdrift from the eroding face. The alongshore displacement of the subaerial center of mass of the 2012 nourishments is positively correlated with the seasonally varying (the alongshore radiation stress component). After four years, the net southward drift of the Imperial Beach nourishment contributed to the winter 2016 closure of the Tijuana River mouth and the associated hyper-polluted and anoxic estuary conditions. Nourishment impacts on sand levels on rocky reefs were not unambiguously detectable in the background of natural variability. Over several years, gains or losses in the total sand volume (integrated from the back beach to 8 m depth, over the few km alongshore survey spans) are sometimes comparable to nourishment volumes, suggesting relatively large interannual sediment fluxes across the control volume boundaries. The clearest trend in total volume is at Torrey Pines; during 16 years since the 2001 nourishment, about 300,000 m3 of sand has been lost. If the trend continues, the thinning veneer of sand will be removed more often from the subaerial winter beach, exposing rocks and cobbles.
Keywords:
[+]
Beaches Coast Changes Sand replenishment
Source:
Coastal Engineering 136: 96-105
DOI:
https://doi.org/10.1016/j.coastaleng.2018.02.003
Sea Grant Document Number:
CASG-R-18-015
Document Type:
Journal Article
Funding:
Grant no. NA10OAR4170060
Place as Subject:
California, Southern
Rights Information:
CC BY-NC-ND
Compliance:
Library
Main Document Checksum:
[+]
urn:sha256:19bdc9c93bc25100076616ce52f7cb90b0475ad655f9345ee8e79a4de32779c5
Download URL:
https://repository.library.noaa.gov/view/noaa/43789/noaa_43789_DS1.pdf
File Type:

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