Coastal flooding and the 1861-2 California storm season

Laura C. Reynolds, Alexander R. Simms, Ana Ejarque, Baird King, R. Scott Anderson, Joseph A. Carlin, J. Michael Bentz, Thomas K. Rockwell, Robert Peters

Research output: Contribution to journalArticle

2 Scopus citations

Abstract

A series of large storms attributed to Atmospheric River conditions struck the California coast in the winter of 1861-2. Although historical accounts document inland flooding, little is known about how the 1861-2 storms impacted the now heavily-developed California coast. Here we show that the 1861-2 storms emplaced a deposit of beach sand up to 50 cm thick over 450 m inland within a southern California salt marsh. This deposit is unprecedented in the post-European sediments of the marsh and more extensive than that derived from any other historical event. It is comparable in scale to hurricane and tsunami washover fans in back-barrier environments along other coastlines. The presence of overwash deposits in Carpinteria suggests that the 1861-2 storm season was erosive enough to remove coastal barriers, allowing for inundation of parts of the coastline currently developed. Efforts to prepare for a recurrence of an 1861-2-like storm season should address potential coastal impacts; likewise, interpretations of past washover deposits should consider these unusually prolonged stormy periods in addition to hurricane and tsunami inundation.

Original languageEnglish (US)
Pages (from-to)49-59
Number of pages11
JournalMarine Geology
Volume400
DOIs
StatePublished - Jun 1 2018

Keywords

  • Atmospheric rivers
  • Estuaries (morphology and stratigraphy)
  • Estuarine processes
  • Geochronology
  • NE Pacific
  • Storms and their deposits

ASJC Scopus subject areas

  • Oceanography
  • Geology
  • Geochemistry and Petrology

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  • Cite this

    Reynolds, L. C., Simms, A. R., Ejarque, A., King, B., Anderson, R. S., Carlin, J. A., Bentz, J. M., Rockwell, T. K., & Peters, R. (2018). Coastal flooding and the 1861-2 California storm season. Marine Geology, 400, 49-59. https://doi.org/10.1016/j.margeo.2018.02.005