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    Statistics of Internal Tide Bores and Internal Solitary Waves Observed on the Inner Continental Shelf off Point Sal, California

    Source: Journal of Physical Oceanography:;2017:;volume 048:;issue 001::page 123
    Author:
    Colosi, John A.
    ,
    Kumar, Nirnimesh
    ,
    Suanda, Sutara H.
    ,
    Freismuth, Tucker M.
    ,
    MacMahan, Jamie H.
    DOI: 10.1175/JPO-D-17-0045.1
    Publisher: American Meteorological Society
    Abstract: AbstractMoored observations of temperature and current were collected on the inner continental shelf off Point Sal, California, between 9 June and 8 August 2015. The measurements consist of 10 moorings in total: 4 moorings each on the 50- and 30-m isobaths covering a 10-km along-shelf distance and an across-shelf section of moorings on the 50-, 40-, 30-, and 20-m isobaths covering a 5-km distance. Energetic, highly variable, and strongly dissipating transient wave events termed internal tide bores and internal solitary waves (ISWs) dominate the records. Simple models of the bore and ISW space?time behavior are implemented as a temperature match filter to detect events and estimate wave packet parameters as a function of time and mooring position. Wave-derived quantities include 1) group speed and direction; 2) time of arrival, time duration, vertical displacement amplitude, and waves per day; and 3) energy density, energy flux, and propagation loss. In total, over 1000 bore events and over 9000 ISW events were detected providing well-sampled statistical distributions. Statistics of the waves are rather insensitive to position along shelf but change markedly in the across-shelf direction. Two compelling results are 1) that the probability density functions for bore and ISW energy flux are nearly exponential, suggesting the importance of interference and 2) that wave propagation loss is proportional to energy flux, thus giving an exponential decay of energy flux toward shore with an e-folding scale of 2?2.4 km and average dissipation rates for bores and ISWs of 144 and 1.5 W m?1, respectively.
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      Statistics of Internal Tide Bores and Internal Solitary Waves Observed on the Inner Continental Shelf off Point Sal, California

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4260846
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    • Journal of Physical Oceanography

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    contributor authorColosi, John A.
    contributor authorKumar, Nirnimesh
    contributor authorSuanda, Sutara H.
    contributor authorFreismuth, Tucker M.
    contributor authorMacMahan, Jamie H.
    date accessioned2019-09-19T10:02:16Z
    date available2019-09-19T10:02:16Z
    date copyright8/29/2017 12:00:00 AM
    date issued2017
    identifier otherjpo-d-17-0045.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4260846
    description abstractAbstractMoored observations of temperature and current were collected on the inner continental shelf off Point Sal, California, between 9 June and 8 August 2015. The measurements consist of 10 moorings in total: 4 moorings each on the 50- and 30-m isobaths covering a 10-km along-shelf distance and an across-shelf section of moorings on the 50-, 40-, 30-, and 20-m isobaths covering a 5-km distance. Energetic, highly variable, and strongly dissipating transient wave events termed internal tide bores and internal solitary waves (ISWs) dominate the records. Simple models of the bore and ISW space?time behavior are implemented as a temperature match filter to detect events and estimate wave packet parameters as a function of time and mooring position. Wave-derived quantities include 1) group speed and direction; 2) time of arrival, time duration, vertical displacement amplitude, and waves per day; and 3) energy density, energy flux, and propagation loss. In total, over 1000 bore events and over 9000 ISW events were detected providing well-sampled statistical distributions. Statistics of the waves are rather insensitive to position along shelf but change markedly in the across-shelf direction. Two compelling results are 1) that the probability density functions for bore and ISW energy flux are nearly exponential, suggesting the importance of interference and 2) that wave propagation loss is proportional to energy flux, thus giving an exponential decay of energy flux toward shore with an e-folding scale of 2?2.4 km and average dissipation rates for bores and ISWs of 144 and 1.5 W m?1, respectively.
    publisherAmerican Meteorological Society
    titleStatistics of Internal Tide Bores and Internal Solitary Waves Observed on the Inner Continental Shelf off Point Sal, California
    typeJournal Paper
    journal volume48
    journal issue1
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-17-0045.1
    journal fristpage123
    journal lastpage143
    treeJournal of Physical Oceanography:;2017:;volume 048:;issue 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian