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Zhu, Qiang 1970. "Features of nonlinear wave-wave and wave-body interactions". Thesis, Massachusetts Institute of Technology, 2000. http://hdl.handle.net/1721.1/8853.
Pełny tekst źródłaIncludes bibliographical references (leaves 295-302).
Although nonlinear water waves have been the subject of decades of research, there are many problems that remain unsolved, especially in the cases when one or more of the following factors are involved: high-order nonlinear effects, moving boundaries, wavestructure interactions and complicated geometries. In this dissertation, a high-order spectral-element (HOSE) method is developed to investigate problems about nonlinear waves. An exponentially converging algorithm, it is able to be applied to solve nonlinear interactions between waves and submerged or surface-piercing bodies with high-order nonlinear effects. The HOSE method is applied to investigate dynamics of nonlinear waves and their interactions with obstacles. We first implement it to calculate the hydrodynamic forces and moments on a fixed underwater spheroid, with uniform current, different angles of attack and finite water depth included in the study. Extending this study to wave interaction with tethered bodies, we create an efficient simulation capability of moored buoys. Coupling the HOSE method with a robust implicit finite-difference solver of highly-extensible cables, our results show chaotic buoy motions and the ability for short wave generation. We then focus our attention on the free-surface patterns caused by nonlinear wave-wave and wave-body interactions. Starting with a two-dimensional canonical problem about the wave diffraction and radiation of a submerged circular cylinder, numerical evidences are obtained to corroborate that, for a fixed cylinder, a cylinder undergoing forced circular motion, or free to respond to incident waves, the progressive disturbances are in one direction only. The three-dimensional wave-wave interactions are studied. It is proved both analytically and numerically that new propagating waves could be generated by the resonant interactions between Kelvin ship waves and ambient waves. Another consequence of resonant wave-wave interactions is the instability of free-surface waves. In this dissertation, the three-dimensional unstable modes of plane standing waves and standing waves in a circular basin are identified numerically and then confirmed analytically. These investigations cover a large variety of nonlinear-wave problems and prove that the HOSE method is an efficient tool in studying scientific or practical problems.
by Qiang Zhu.
Ph.D.
Naciri, Mamoun. "On wave-wave interactions on the ocean surface". Thesis, Massachusetts Institute of Technology, 1992. http://hdl.handle.net/1721.1/47312.
Pełny tekst źródłaYu, Sihan. "Ocean Wave Simulation and Prediction". Thesis, Virginia Tech, 2018. http://hdl.handle.net/10919/84992.
Pełny tekst źródłaMaster of Science
Greenwood, Charles. "The impact of large scale wave energy converter farms on the regional wave climate". Thesis, University of the Highlands and Islands, 2016. https://pure.uhi.ac.uk/portal/en/studentthesis/the-impact-of-large-scale-wave-energy-converter-farms-on-the-regional-wave-climate(e734db00-2108-48f9-b162-a1fc85ef61d6).html.
Pełny tekst źródłaScott, Nicholas Vicente. "Observations of the wind-wave spectrum and steep wave statistics in open ocean waters". View online ; access limited to URI, 2003. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3103724.
Pełny tekst źródłaSuoja, Nicole Marie. "Development of a directional wave gage for short sea waves". Thesis, Massachusetts Institute of Technology, 1996. http://hdl.handle.net/1721.1/38163.
Pełny tekst źródłaHenry, Legena Albertha. "A study of ocean wave statistical properties using nonlinear, directional, phase-resolved ocean wave-field simulations". Thesis, Massachusetts Institute of Technology, 2009. http://hdl.handle.net/1912/3230.
Pełny tekst źródłaCataloged from PDF version of thesis.
Includes bibliographical references (p. 327-334).
In the present work, we study the statistics of wavefields obtained from non-linear phase-resolved simulations. The numerical model used to generate the waves models wave-wave interactions based on the fully non-linear Zakharov equations. We vary the simulated wavefield's input spectral properties: directional spreading function, Phillips parameter and peak shape parameter. We then investigate the relationships between a wavefield's input spectral properties and its output physical properties via statistical analysis. We investigate surface elevation distribution, wave definition methods in a nonlinear wavefield with a two-dimensional wavenumber, defined waves' distributions, and the occurrence and spacing of large wave events.
by Legena Albertha Henry.
S.M.
Xue, Ming 1967. "Three-dimensional fully-nonlinear simulations of waves and wave body interactions". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/10216.
Pełny tekst źródłaProehl, Jeffrey A. "Equatorial wave-mean flow interaction : the long Rossby waves /". Thesis, Connect to this title online; UW restricted, 1988. http://hdl.handle.net/1773/10960.
Pełny tekst źródłaGuo, Y. P. "Wave-induced sound in the ocean". Thesis, University of Cambridge, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.384781.
Pełny tekst źródłaRahm, Magnus. "Ocean Wave Energy : Underwater Substation System for Wave Energy Converters". Doctoral thesis, Uppsala universitet, Elektricitetslära, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-112915.
Pełny tekst źródłaSemedo, Alvaro. "Atmosphere-ocean Interactions in Swell Dominated Wave Fields". Doctoral thesis, Uppsala universitet, Geovetenskapliga sektionen, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-130650.
Pełny tekst źródłaGränsen mellan hav och atmosfär beskrivs av vågor, dessa spelar en central roll i utbytesprocesser mellan hav och atmosfär. Värme, massa och rörelsemängd överförs vid ytan och utbytet av rörelsemängd mellan vind och havsyta styrs i stor utsträckning av vågorna. Då vågor skapas kallas de för vinddrivna vågor. När vågorna sedan lämnar området där de genererats eller rör sig fortare än den vind som genererat dem kallas de dyning. Ett vågfält kan sägas vara dominerat av antingen vinddrivna vågor eller dyningsvågor. Beroende på vilken vågregim som råder så är kopplingen mellan vågor och vind olika och därmed också utbytesprocesserna för rörelsemängd och energi. Då vågorna genereras fungerar de som en bromsande kraft för vinden och impulsutbytet är nedåtriktat. När dyning dominerar vågfältet inträffar en mekanism för omvänt impulsutbyte som sätts igång av dyningsvågor som färdas avsevärt snabbare än vinden. Rörelsemängd överförs då från vågorna till atmosfären, eftersom dyningsvågorna utför arbete på atmosfären då de dämpas. Den uppåtriktade transporten av rörelsemängd har en stor effekt på dynamiken och turbulensstrukturen i lägre delen av atmosfären. En detaljerad kvalitativ klimatologi av globala vågfält (vinddrivna och dyning) från återanalysdata presenteras och visar att dyning dominerar vågfältet på världshaven. Områden där man kan förvänta sig störst effekt av dyning på atmosfären har identifierats. En konceptuellt baserad modell som reproducerar effekten av dyning på dynamiken i lägre delen av atmosfären presenteras. Modellen styrs av överföring av energi från vågor till atmosfären. I modellen föreslås även en ny parameterisering för våginducerad kraft på havsytan. Modellresultaten är utvärderade mot fältmätningar. En regional klimatmodell, med ett kopplat våg-atmosfärssystem, har använts för att studera den långtida effekten av dyning vid klimatsimulering. Olika formuleringar för beskrivningen av vågornas effekt på atmosfären har använts, beroende på om vinddrivna vågor eller dyning dominerar vågfältet.
Ray, Timothy Allen. "Wave propagation over complex bathymetry". Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03Jun%5FRay.pdf.
Pełny tekst źródłaThesis advisor(s): Thomas H.C. Herbers, Edward B. Thornton. Includes bibliographical references (p. 37). Also available online.
Chen, David Joel. "Designing wave-measuring instruments". Thesis, Massachusetts Institute of Technology, 1994. http://hdl.handle.net/1721.1/12108.
Pełny tekst źródłaWu, Cheng Y. (Cheng Yi) 1938. "Wave-wave interactions and the infrasonic pressure field in the ocean". Thesis, University of Auckland, 1988. http://hdl.handle.net/2292/2469.
Pełny tekst źródłaWist, Hanne Therese. "Statistical properties of successive ocean wave parameters". Doctoral thesis, Norwegian University of Science and Technology, Norwegian University of Science and Technology, 2003. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-16.
Pełny tekst źródłaFor random waves the free surface elevation can be described by a number of individual wave parameters. The main objective of this work has been to study the statistical properties of individual parameters in successive waves; the wave crest height, the wave height and the wave period.
In severe sea states the wave crest heights exhibit a nonlinear behavior, which must be reflected in the models. An existing marginal distribution that uses second order Stokes-type nonlinearity is transformed to a two-dimensional distribution by use of the two–dimensional Rayleigh distribution. This model only includes sum frequency effects. A two-dimensional distribution is also established by transforming a second order model including both sum and different frequency effects. Both models are based on the narrow-band assumption, and the effect of finite water depth is included. A parametric wave crest height distribution proposed by Forristall (2000) has been extended to two dimensions by transformation of the two-dimensional Weibull distribution.
Two successive wave heights are modeled by a Gaussian copula, which is referred to as the Nataf model. Results with two initial distributions for the transformation are presented, the Næss (1985) model and a two-parameter Weibull distribution, where the latter is in best agreement with data. The results are compared with existing models. The Nataf model has also been used for modeling three successive wave heights. Results show that the Nataf transformation of three successive wave heights can be approximated by a first order autoregression model. This means that the distribution of the wave height given the previous wave height is independent of the wave heights prior to the previous wave height. The simulation of successive wave heights can be done directly without simulating the time series of the complete surface elevation.
Successive wave periods are modeled with the Nataf transformation by using a two-parameter Weibull distribution and a generalized Gamma distribution as the initial distribution, where the latter is in best agreement with data. Results for the marginal and two-dimensional distributions are compared with existing models. In practical applications, it is often of interest to consider successive wave periods with corresponding wave heights exceeding a certain threshold. Results show that the distribution for successive wave periods when the corresponding wave heights exceed the root-mean-square value of the wave heights can be approximated by a multivariate Gaussian distribution. When comparing the results with data, a long time series is needed in order to obtain enough data cases. Results for three successive wave periods are also presented.
The models are compared with field data from the Draupner field and the Japan Sea, and with laboratory data from experiments at HR Wallingford. In addition, data from numerical simulations based on second order wave theory, including both sum and frequency effects, are included.
Patoux, Jérôme. "Frontal wave development over the Southern Ocean /". Thesis, Connect to this title online; UW restricted, 2003. http://hdl.handle.net/1773/10067.
Pełny tekst źródłaMelo, Jose Luis Branco Seabra de. "Nonlinear parametric wave model compared with field data". Monterey, Calif. : Naval Postgraduate School, 1985. http://catalog.hathitrust.org/api/volumes/oclc/57738811.html.
Pełny tekst źródłaWalker, Daniel Anthony Guy. "Interaction of extreme ocean waves with offshore structures". Thesis, University of Oxford, 2006. http://ora.ox.ac.uk/objects/uuid:6858dc08-1bd4-4195-8893-1af98d5e68e3.
Pełny tekst źródłaSweeny, Margaret E. "Breaking wave turbulence in the surf zone". Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05Jun%5FSweeny.pdf.
Pełny tekst źródłaThesis Advisor(s): Timothy P. Stanton. Includes bibliographical references (p. 51). Also available online.
Cohen, Jennifer Esther. "Theory of turbulent wind over fast and slow waves". Thesis, University of Cambridge, 1997. https://www.repository.cam.ac.uk/handle/1810/283717.
Pełny tekst źródłaKlepsvik, Jonny. "Nonlinear wave loads on offshore structures". Thesis, Massachusetts Institute of Technology, 1995. http://hdl.handle.net/1721.1/36062.
Pełny tekst źródłaMurphy, Darryl Guy. "Rossby waves in the Southern Ocean". Thesis, University of Exeter, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303178.
Pełny tekst źródłaAbdelrahman, Saad M. M. "Shore wave modulation due to infragravity waves in the nearshore zone, with applications". Monterey, Calif. : Naval Postgraduate School, 1986. http://catalog.hathitrust.org/api/volumes/oclc/57743239.html.
Pełny tekst źródłaXu, Xu. "Nonlinear dynamics of parametric pendulum for wave energy extraction". Thesis, University of Aberdeen, 2005. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=189414.
Pełny tekst źródłaPeak, Scott Douglas. "Wave refraction over complex nearshore bathymetry". Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2004. http://library.nps.navy.mil/uhtbin/hyperion/04Dec%5FPeak.pdf.
Pełny tekst źródłaHarlander, Uwe, i Werner Metz. "Rossby wave propagation in a bounded ocean current". Universitätsbibliothek Leipzig, 2016. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-213459.
Pełny tekst źródłaWe study the propagation and the structural change of quasi geostrophic Rossby wave packets by means of a WKB-method. Our approach involves the introduction of a rigid boundary, where the wave packets can be refiected elastically. We study Rossby wave packet dynamics at high latitudes on a modified ß-plane, where the second derivative of the Coriolis parameter with respect to latitude is taken into account (d-term). We show that under certain conditions synoptic-scale wave packets can propagate far distances along an east-west oriented \"coast\" and may affect the fiow far downstream of the source region. In contrast to free propagating Rossby wave packets ( e.g. in the atmosphere), which can be trapped between two turning latitudes, the wave packets considered here are trapped between a turning latitude and the reflecting boundary. lt turns out that the 6-term is most important for wave packets with negative phase speeds. Finally, we suggest that such a selective Rossby waveguide may play a role in the dynamics of the Antarctic Circumpolar Current
Joubert, J. R. "An investigation of the wave energy resource on the South African Coast, focusing on the spatial distribution of the South West coast". Thesis, Link to the Internet, 2008. http://hdl.handle.net/10019.1/351.
Pełny tekst źródłaStorie, Eric S. "Multi-fractal analysis of SAR ocean wave imagery". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0014/MQ36849.pdf.
Pełny tekst źródłaNavarro, Moisés M. "Ocean wave data analysis using Hilbert transform techniques". Thesis, Monterey, California. Naval Postgraduate School, 1996. http://hdl.handle.net/10945/32022.
Pełny tekst źródłaTang, Dajun. "Acoustic wave scattering from a random ocean bottom". Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/13908.
Pełny tekst źródłaIncludes bibliographical references (leaves 123-130).
Dajun Tang.
Ph.D.
Harlander, Uwe, i Werner Metz. "Rossby wave propagation in a bounded ocean current". Wissenschaftliche Mitteilungen des Leipziger Instituts für Meteorologie ; 9 = Meteorologische Arbeiten aus Leipzig ; 3 (1998), S. 130-147, 1998. https://ul.qucosa.de/id/qucosa%3A15085.
Pełny tekst źródłaWe study the propagation and the structural change of quasi geostrophic Rossby wave packets by means of a WKB-method. Our approach involves the introduction of a rigid boundary, where the wave packets can be refiected elastically. We study Rossby wave packet dynamics at high latitudes on a modified ß-plane, where the second derivative of the Coriolis parameter with respect to latitude is taken into account (d-term). We show that under certain conditions synoptic-scale wave packets can propagate far distances along an east-west oriented \"coast\" and may affect the fiow far downstream of the source region. In contrast to free propagating Rossby wave packets ( e.g. in the atmosphere), which can be trapped between two turning latitudes, the wave packets considered here are trapped between a turning latitude and the reflecting boundary. lt turns out that the 6-term is most important for wave packets with negative phase speeds. Finally, we suggest that such a selective Rossby waveguide may play a role in the dynamics of the Antarctic Circumpolar Current.
Orszaghova, Jana. "Solitary waves and wave groups at the shore". Thesis, University of Oxford, 2011. http://ora.ox.ac.uk/objects/uuid:5b168bdc-4956-4152-a303-b23a6067bf42.
Pełny tekst źródłaWhitford, Dennis James. "Wind and wave forcing of longshore currents across a barred beach". Thesis, Monterey, Calif. : Naval Postgraduate School, 1988. http://catalog.hathitrust.org/api/volumes/oclc/52803820.html.
Pełny tekst źródłaWaters, Rafael. "Energy from Ocean Waves : Full Scale Experimental Verification of a Wave Energy Converter". Doctoral thesis, Uppsala universitet, Elektricitetslära, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-9404.
Pełny tekst źródłaNoad, Imogen Frances. "Absorbing power from ocean waves : a mathematical approach to modelling wave energy converters". Thesis, University of Bristol, 2018. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.752773.
Pełny tekst źródłaLi, Wei. "Numerical Modelling and Statistical Analysis of Ocean Wave Energy Converters and Wave Climates". Doctoral thesis, Uppsala universitet, Elektricitetslära, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-305870.
Pełny tekst źródłaBoyd, Jeremy David. "Evaluation of ADCP wave measurements". Thesis, Monterey, Calif. : Naval Postgraduate School, 2006. http://bosun.nps.edu/uhtbin/hyperion.exe/06Dec%5FBoydE.pdf.
Pełny tekst źródłaThesis Advisor(s): Thomas H.C. Herbers. "December 2006." Includes bibliographical references (p. 51-52). Also available in print.
Morris-Thomas, Michael. "An investigation into wave run-up on vertical surface piercing cylinders in monochromatic waves". University of Western Australia. School of Oil and Gas Engineering, 2003. http://theses.library.uwa.edu.au/adt-WU2004.0010.
Pełny tekst źródłaAlves, Jose Henrique Gomes de Mattos Mathematics UNSW. "A Saturation-Dependent Dissipation Source Function for Wind-Wave Modelling Applications". Awarded by:University of New South Wales. Mathematics, 2000. http://handle.unsw.edu.au/1959.4/17786.
Pełny tekst źródłaBallard, Valerie Jean. "Experiments with a high frequency laser slope meter". Thesis, University of Southampton, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367969.
Pełny tekst źródłaMagagna, Davide. "Oscillating water column wave pump : a wave energy converter for water delivery". Thesis, University of Southampton, 2011. https://eprints.soton.ac.uk/349009/.
Pełny tekst źródłaLee, Hyun Yup. "Drillstring axial vibration and wave propagation in boreholes". Thesis, Massachusetts Institute of Technology, 1991. http://hdl.handle.net/1721.1/13907.
Pełny tekst źródłaVan, der Westhuysen A. J. "The application of the numerical wind wave model SWAN to a selected field case on the South African coast". Thesis, Link to the online version, 2002. http://hdl.handle.net/10019.1/3632.
Pełny tekst źródłaMcAllister, Mark Laing. "Analysis of laboratory and field measurements of directionally spread nonlinear ocean waves". Thesis, University of Edinburgh, 2017. http://hdl.handle.net/1842/28762.
Pełny tekst źródłaQin, Wenting. "Application of the spectral wave model SWAN in Delaware Bay". Access to citation, abstract and download form provided by ProQuest Information and Learning Company; downloadable PDF file 4.68 Mb., 130 p, 2005. http://proquest.umi.com/pqdlink?did=1037889341&Fmt=7&clientId=8331&RQT=309&VName=PQD.
Pełny tekst źródłaCureton, Geoffrey Patrick. "Retrieval of nonlinear spectral information from ocean sunglint". Thesis, Curtin University, 2010. http://hdl.handle.net/20.500.11937/1549.
Pełny tekst źródłaWallace, Stephanie. "The relationship between ocean wave statistics and satellite measurements". Thesis, The University of Sydney, 1993. https://hdl.handle.net/2123/26654.
Pełny tekst źródłaSiddorn, Philip David. "Efficient numerical modelling of wave-structure interaction". Thesis, University of Oxford, 2012. http://ora.ox.ac.uk/objects/uuid:de36bd2f-cd23-4f11-b67f-9d8cd48ecd3c.
Pełny tekst źródłaBrookins, A. Henry. "Ocean wave height transformation model using surface roller theory". Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1993. http://handle.dtic.mil/100.2/ADA272610.
Pełny tekst źródła