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Mid‐El Niño erosion at nourished and unnourished Southern California beaches
Author(s) -
Ludka B. C.,
Gallien T. W.,
Crosby S. C.,
Guza R. T.
Publication year - 2016
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1002/2016gl068612
Subject(s) - subaerial , shore , erosion , storm , beach nourishment , geology , coastal erosion , oceanography , geography , physical geography , hydrology (agriculture) , geomorphology , geotechnical engineering , paleontology
Wave conditions in Southern California during the 2015–2016 El Niño were similar to the 2009–2010 El Niño, previously the most erosive (minimum beach widths and subaerial sand levels) in a 7 year record. As of February 2016, Torrey Pines Beach had eroded slightly below 2009–2010 levels, threatening the shoulder of a major highway. However, Cardiff, Solana, and Imperial Beaches, nourished with imported sand in 2012, were on average 1–2 m more elevated and more than 10 m wider than in 2009–2010. Monthly subaerial sand elevation observations showed that the nourished beaches remained consistently wider than unnourished beaches under similar wave conditions. In contrast to a 2001 nourishment at Torrey Pines built with native sized sand that was removed from the beach face during a single storm, these relatively coarse grained nourishments protected shorelines for several years, and during the significant wave attack of the 2015–2016 El Niño, as of February 2016.