4.5 Article

A regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes

期刊

EARTH SURFACE PROCESSES AND LANDFORMS
卷 43, 期 12, 页码 2562-2577

出版社

WILEY
DOI: 10.1002/esp.4415

关键词

natural hazards; suspended sediment; sediment load; floods; coastal watershed; climate change; extreme events

资金

  1. Coastal and Marine Geology Program of the US Geological Survey

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Small, steep watersheds are prolific sediment sources from which sediment flux is highly sensitive to climatic changes. Storm intensity and frequency are widely expected to increase during the 21st century, and so assessing the response of small, steep watersheds to extreme rainfall is essential to understanding landscape response to climate change. During record winter rainfall in 2016-2017, the San Lorenzo River, coastal California, had nine flow peaks representing 2-10-year flood magnitudes. By the third flood, fluvial suspended sediment showed a regime shift to greater and coarser sediment supply, coincident with numerous landslides in the watershed. Even with no singular catastrophic flood, these flows exported more than half as much sediment as had a 100-year flood 35years earlier, substantially enlarging the nearshore delta. Annual sediment load in 2017 was an order of magnitude greater than during an average-rainfall year, and 500-fold greater than in a recent drought. These anomalous sediment inputs are critical to the coastal littoral system, delivering enough sediment, sometimes over only a few days, to maintain beaches for several years. Future projections of megadroughts punctuated by major atmospheric-river storm activity suggest that interannual sediment-yield variations will become more extreme than today in the western USA, with potential consequences for coastal management, ecosystems, and water-storage capacity. The occurrence of two years with major sediment export over the past 35years that were not associated with extremes of the El Nino Southern Oscillation or Pacific Decadal Oscillation suggests caution in interpreting climatic signals from marine sedimentary deposits derived from small, steep, coastal watersheds, to avoid misinterpreting the frequencies of those cycles. Published 2018. This article is a U.S. Government work and is in the public domain in the USA.

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