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Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California.

紀錄類型:	書目-電子資源 : Monograph/item
正題名/作者:	Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California./
作者:	Storlazzi, Curt Daron.
面頁冊數:	1 online resource (139 pages)
附註:	Source: Dissertations Abstracts International, Volume: 62-05, Section: B.
Contained By:	Dissertations Abstracts International62-05B.
標題:	Geology. -
電子資源:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9979947click for full text (PQDT)
ISBN:	9780599856912

Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California.
Storlazzi, Curt Daron.

Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California. - 1 online resource (139 pages)

Source: Dissertations Abstracts International, Volume: 62-05, Section: B.

Thesis (Ph.D.)--University of California, Santa Cruz, 2000.

Includes bibliographical references

Records from Peru documenting the effects of one side of the Southern Oscillation, 'El Nino-Southern Oscillation' (ENSO), have stretched back for centuries: however, there is little evidence that this large-scale oscillation has historically affected the coast of central California. It is shown that ENSOs, especially intense ENSO events, produce higher waves and sea level, heavier precipitation, and more cyclones and local storms than normal along the central coast. The Southern Oscillation, thought to only affect low latitudes, significantly influences the timing and magnitude of storms that strike central California. It appears that the frequency and intensity of ENSO events exert primary control on the geomorphologic evolution of central California's shoreline. It was shown that the geology and structure are the main controls on the distribution of sediment in rocky nearshores as they define the patterns through which rivers and stream incise over the course of sea level fluctuations. Paleo-stream channels incised on the shoreface are depressed below the surrounding bedrock; thus, headlands extend offshore as bedrock ridges and stream channels are fronted by sediment-tilled depressions. This high bathymetric relief suggests that large waves are needed to suspended sediment high enough off the bed to be transported over the bedrock ridges. Thus, timing and magnitude of sediment transport along rocky shorelines is strongly dependent on the frequency and magnitude of energetic storms, much more so than along the planar, sandy shorelines. An instrument was deployed in a paleo-stream channel off a pocket beach north of Santa Cruz, California. This environment was energetic and wave-orbital motions dominated the near-bed flow. Intermittent, intense periods of sediment suspension were correlated with large waves and wave groups. Over 9500 sediment suspension events (SSEs) occurred. SSEs are shown to contribute almost 100% of the total sediment suspended during storms, demonstrating the importance of these events to sediment transport. Shelf sediment transport models cannot accurately model the magnitude and direction of sediment transport on this shoreface due to the lack of information regarding the instantaneous coupling between fluid flow and sediment suspension. Time-variant models must be developed to accurately model sediment transport in this type of environment.

Electronic reproduction.
Ann Arbor, Mich. :
ProQuest,
2023

Mode of access: World Wide Web

ISBN: 9780599856912Subjects--Topical Terms:

516570
Geology.
Subjects--Index Terms:

CaliforniaIndex Terms--Genre/Form:

542853
Electronic books.

Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California.
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245 1 0 $a Hydrodynamics, sediment transport, and El Nino-induced seacliff erosion along the coastline of central California.
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500 $a Source: Dissertations Abstracts International, Volume: 62-05, Section: B.
500 $a Publisher info.: Dissertation/Thesis.
500 $a Advisor: Griggs, Gary B.
502 $a Thesis (Ph.D.)--University of California, Santa Cruz, 2000.
504 $a Includes bibliographical references
520 $a Records from Peru documenting the effects of one side of the Southern Oscillation, 'El Nino-Southern Oscillation' (ENSO), have stretched back for centuries: however, there is little evidence that this large-scale oscillation has historically affected the coast of central California. It is shown that ENSOs, especially intense ENSO events, produce higher waves and sea level, heavier precipitation, and more cyclones and local storms than normal along the central coast. The Southern Oscillation, thought to only affect low latitudes, significantly influences the timing and magnitude of storms that strike central California. It appears that the frequency and intensity of ENSO events exert primary control on the geomorphologic evolution of central California's shoreline. It was shown that the geology and structure are the main controls on the distribution of sediment in rocky nearshores as they define the patterns through which rivers and stream incise over the course of sea level fluctuations. Paleo-stream channels incised on the shoreface are depressed below the surrounding bedrock; thus, headlands extend offshore as bedrock ridges and stream channels are fronted by sediment-tilled depressions. This high bathymetric relief suggests that large waves are needed to suspended sediment high enough off the bed to be transported over the bedrock ridges. Thus, timing and magnitude of sediment transport along rocky shorelines is strongly dependent on the frequency and magnitude of energetic storms, much more so than along the planar, sandy shorelines. An instrument was deployed in a paleo-stream channel off a pocket beach north of Santa Cruz, California. This environment was energetic and wave-orbital motions dominated the near-bed flow. Intermittent, intense periods of sediment suspension were correlated with large waves and wave groups. Over 9500 sediment suspension events (SSEs) occurred. SSEs are shown to contribute almost 100% of the total sediment suspended during storms, demonstrating the importance of these events to sediment transport. Shelf sediment transport models cannot accurately model the magnitude and direction of sediment transport on this shoreface due to the lack of information regarding the instantaneous coupling between fluid flow and sediment suspension. Time-variant models must be developed to accurately model sediment transport in this type of environment.
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538 $a Mode of access: World Wide Web
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650 4 $a Oceanography. $3 535383
650 4 $a Environmental science. $3 677245
650 4 $a Geography. $3 524010
650 4 $a Physical oceanography. $3 3168433
650 4 $a Physical geography. $3 516662
653 $a California
653 $a Coastline
653 $a El Nino-Southern Oscillation
653 $a Erosion
653 $a Hydrodynamics
653 $a Seacliff
653 $a Sediment transport
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773 0 $t Dissertations Abstracts International $g 62-05B.
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9979947 $z click for full text (PQDT)