FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2802821093> ?p ?o ?g. }

• W2802821093 endingPage "2577" @default.
• W2802821093 startingPage "2562" @default.
• W2802821093 abstract "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 35 years 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 35 years that were not associated with extremes of the El Niño 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." @default.
• W2802821093 created "2018-05-17" @default.
• W2802821093 creator A5008083062 @default.
• W2802821093 creator A5024687097 @default.
• W2802821093 creator A5036216831 @default.
• W2802821093 creator A5063739074 @default.
• W2802821093 creator A5064449973 @default.
• W2802821093 creator A5091166278 @default.
• W2802821093 creator A5091177095 @default.
• W2802821093 date "2018-06-19" @default.
• W2802821093 modified "2023-09-27" @default.
• W2802821093 title "A regime shift in sediment export from a coastal watershed during a record wet winter, California: Implications for landscape response to hydroclimatic extremes" @default.
• W2802821093 cites W149809181 @default.
• W2802821093 cites W1519584274 @default.
• W2802821093 cites W1529582850 @default.
• W2802821093 cites W1543206423 @default.
• W2802821093 cites W1555473120 @default.
• W2802821093 cites W1605954873 @default.
• W2802821093 cites W1656732585 @default.
• W2802821093 cites W1733550608 @default.
• W2802821093 cites W1780635652 @default.
• W2802821093 cites W1795838465 @default.
• W2802821093 cites W1798418024 @default.
• W2802821093 cites W1821436614 @default.
• W2802821093 cites W1886700992 @default.
• W2802821093 cites W1913143193 @default.
• W2802821093 cites W1919969435 @default.
• W2802821093 cites W1963790290 @default.
• W2802821093 cites W1966076903 @default.
• W2802821093 cites W1969302920 @default.
• W2802821093 cites W1970010064 @default.
• W2802821093 cites W1970130975 @default.
• W2802821093 cites W1973024791 @default.
• W2802821093 cites W1973530684 @default.
• W2802821093 cites W1974355959 @default.
• W2802821093 cites W1982182456 @default.
• W2802821093 cites W1987595445 @default.
• W2802821093 cites W1988837933 @default.
• W2802821093 cites W1990830084 @default.
• W2802821093 cites W1993335255 @default.
• W2802821093 cites W1996801857 @default.
• W2802821093 cites W1997897326 @default.
• W2802821093 cites W1999101684 @default.
• W2802821093 cites W2000280421 @default.
• W2802821093 cites W2003161569 @default.
• W2802821093 cites W2010774435 @default.
• W2802821093 cites W2013204779 @default.
• W2802821093 cites W2018346473 @default.
• W2802821093 cites W2020244903 @default.
• W2802821093 cites W2026886308 @default.
• W2802821093 cites W2029343008 @default.
• W2802821093 cites W2037802949 @default.
• W2802821093 cites W2047551560 @default.
• W2802821093 cites W2054101571 @default.
• W2802821093 cites W2063419622 @default.
• W2802821093 cites W2067715694 @default.
• W2802821093 cites W2067758371 @default.
• W2802821093 cites W2071660601 @default.
• W2802821093 cites W2076977109 @default.
• W2802821093 cites W2077249466 @default.
• W2802821093 cites W2081157356 @default.
• W2802821093 cites W2082089934 @default.
• W2802821093 cites W2082425436 @default.
• W2802821093 cites W2099501065 @default.
• W2802821093 cites W2103046654 @default.
• W2802821093 cites W2103688971 @default.
• W2802821093 cites W2104426370 @default.
• W2802821093 cites W2104550434 @default.
• W2802821093 cites W2124664840 @default.
• W2802821093 cites W2130324460 @default.
• W2802821093 cites W2131744835 @default.
• W2802821093 cites W2133154925 @default.
• W2802821093 cites W2142522846 @default.
• W2802821093 cites W2146142479 @default.
• W2802821093 cites W2161251360 @default.
• W2802821093 cites W2168607950 @default.
• W2802821093 cites W2169782692 @default.
• W2802821093 cites W2170418633 @default.
• W2802821093 cites W2198519514 @default.
• W2802821093 cites W2203405612 @default.
• W2802821093 cites W2209096311 @default.
• W2802821093 cites W2209583214 @default.
• W2802821093 cites W2280808532 @default.
• W2802821093 cites W2290693669 @default.
• W2802821093 cites W2303976176 @default.
• W2802821093 cites W2325363144 @default.
• W2802821093 cites W2328474936 @default.
• W2802821093 cites W2328573691 @default.
• W2802821093 cites W2336901076 @default.
• W2802821093 cites W2416160320 @default.
• W2802821093 cites W2463869549 @default.
• W2802821093 cites W2484096247 @default.
• W2802821093 cites W2490312256 @default.
• W2802821093 cites W2499385464 @default.
• W2802821093 cites W2527954392 @default.
• W2802821093 cites W2529168355 @default.
• W2802821093 cites W2588027222 @default.
• W2802821093 cites W2603985521 @default.

• next