FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2154100940> ?p ?o ?g. }

• W2154100940 endingPage "1006" @default.
• W2154100940 startingPage "971" @default.
• W2154100940 abstract "This paper describes a new laboratory study in which a large number of waves, of varying frequency and propagating in different directions, were focused at one point in space and time to produce a large transient wave group. A focusing event of this type is believed to be representative of the evolution of an extreme ocean wave in deep water. Measurements of the water–surface elevation and the underlying water–particle kinematics are compared with both a linear solution and a second–order solution based on the sum of the interactions first identified by Longuet–Higgins & Stewart. Comparisons between these data confirm that the directionality of the wavefield has a profound effect upon the nonlinearity of a large wave event. If the sum of the wave amplitudes generated at the wave paddles is held constant, an increase in the directional spread of the wavefield leads to lower maximum crest elevations. Conversely, if the generated wave amplitudes are increased until the onset of wave breaking, at or near the focal position, an increase in the directional spread allows larger limiting waves to evolve. An explanation of these results lies in the redistribution of the wave energy within the frequency domain. In the most nonlinear wave cases, neither the water–surface elevation nor the water–particle kinematics can be explained in terms of the free waves generated at the wave paddles and their associated bound waves. Indeed, the laboratory data suggest that there is a rapid widening of the free–wave regime in the vicinity of a large wave event. For a constant input–amplitude sum, these important spectral changes are shown to be strongly dependent upon the directionality of the wavefield. These findings explain the very large water–surface elevations recorded in previous unidirectional wave studies and the apparent contrast between unidirectional results and recent field data in which large directionally spread waves were shown to be much less nonlinear. The present study clearly demonstrates the need to incorporate the directionality of a wavefield if extreme ocean waves are to be accurately modelled and their physical characteristics explained." @default.
• W2154100940 created "2016-06-24" @default.
• W2154100940 creator A5022177507 @default.
• W2154100940 creator A5067723525 @default.
• W2154100940 date "2001-04-08" @default.
• W2154100940 modified "2023-10-16" @default.
• W2154100940 title "A laboratory study of the focusing of transient and directionally spread surface water waves" @default.
• W2154100940 cites W1583950238 @default.
• W2154100940 cites W1973464358 @default.
• W2154100940 cites W1991952293 @default.
• W2154100940 cites W2007184676 @default.
• W2154100940 cites W2024624284 @default.
• W2154100940 cites W2031074976 @default.
• W2154100940 cites W2039752589 @default.
• W2154100940 cites W2070526219 @default.
• W2154100940 cites W2071561164 @default.
• W2154100940 cites W2082033753 @default.
• W2154100940 cites W2082105473 @default.
• W2154100940 cites W2092386936 @default.
• W2154100940 cites W2096569922 @default.
• W2154100940 cites W2099317565 @default.
• W2154100940 cites W2104953967 @default.
• W2154100940 cites W2121017288 @default.
• W2154100940 cites W2133382794 @default.
• W2154100940 cites W2140166970 @default.
• W2154100940 cites W2141117243 @default.
• W2154100940 cites W2141791992 @default.
• W2154100940 cites W2160313263 @default.
• W2154100940 cites W2164429670 @default.
• W2154100940 cites W2165532975 @default.
• W2154100940 cites W2172638463 @default.
• W2154100940 cites W50126953 @default.
• W2154100940 doi "https://doi.org/10.1098/rspa.2000.0702" @default.
• W2154100940 hasPublicationYear "2001" @default.
• W2154100940 type Work @default.
• W2154100940 sameAs 2154100940 @default.
• W2154100940 citedByCount "115" @default.
• W2154100940 countsByYear W21541009402012 @default.
• W2154100940 countsByYear W21541009402013 @default.
• W2154100940 countsByYear W21541009402014 @default.
• W2154100940 countsByYear W21541009402015 @default.
• W2154100940 countsByYear W21541009402016 @default.
• W2154100940 countsByYear W21541009402017 @default.
• W2154100940 countsByYear W21541009402018 @default.
• W2154100940 countsByYear W21541009402019 @default.
• W2154100940 countsByYear W21541009402020 @default.
• W2154100940 countsByYear W21541009402021 @default.
• W2154100940 countsByYear W21541009402022 @default.
• W2154100940 countsByYear W21541009402023 @default.
• W2154100940 crossrefType "journal-article" @default.
• W2154100940 hasAuthorship W2154100940A5022177507 @default.
• W2154100940 hasAuthorship W2154100940A5067723525 @default.
• W2154100940 hasConcept C103437262 @default.
• W2154100940 hasConcept C120665830 @default.
• W2154100940 hasConcept C121332964 @default.
• W2154100940 hasConcept C127313418 @default.
• W2154100940 hasConcept C143351421 @default.
• W2154100940 hasConcept C165082838 @default.
• W2154100940 hasConcept C169596890 @default.
• W2154100940 hasConcept C171889981 @default.
• W2154100940 hasConcept C180205008 @default.
• W2154100940 hasConcept C186348155 @default.
• W2154100940 hasConcept C43179477 @default.
• W2154100940 hasConcept C44886760 @default.
• W2154100940 hasConcept C48880136 @default.
• W2154100940 hasConcept C53630964 @default.
• W2154100940 hasConcept C57879066 @default.
• W2154100940 hasConcept C8058405 @default.
• W2154100940 hasConcept C84174578 @default.
• W2154100940 hasConcept C97355855 @default.
• W2154100940 hasConceptScore W2154100940C103437262 @default.
• W2154100940 hasConceptScore W2154100940C120665830 @default.
• W2154100940 hasConceptScore W2154100940C121332964 @default.
• W2154100940 hasConceptScore W2154100940C127313418 @default.
• W2154100940 hasConceptScore W2154100940C143351421 @default.
• W2154100940 hasConceptScore W2154100940C165082838 @default.
• W2154100940 hasConceptScore W2154100940C169596890 @default.
• W2154100940 hasConceptScore W2154100940C171889981 @default.
• W2154100940 hasConceptScore W2154100940C180205008 @default.
• W2154100940 hasConceptScore W2154100940C186348155 @default.
• W2154100940 hasConceptScore W2154100940C43179477 @default.
• W2154100940 hasConceptScore W2154100940C44886760 @default.
• W2154100940 hasConceptScore W2154100940C48880136 @default.
• W2154100940 hasConceptScore W2154100940C53630964 @default.
• W2154100940 hasConceptScore W2154100940C57879066 @default.
• W2154100940 hasConceptScore W2154100940C8058405 @default.
• W2154100940 hasConceptScore W2154100940C84174578 @default.
• W2154100940 hasConceptScore W2154100940C97355855 @default.
• W2154100940 hasIssue "2008" @default.
• W2154100940 hasLocation W21541009401 @default.
• W2154100940 hasOpenAccess W2154100940 @default.
• W2154100940 hasPrimaryLocation W21541009401 @default.
• W2154100940 hasRelatedWork W1490219892 @default.
• W2154100940 hasRelatedWork W1979646715 @default.
• W2154100940 hasRelatedWork W1989925090 @default.
• W2154100940 hasRelatedWork W2009331069 @default.
• W2154100940 hasRelatedWork W2255382471 @default.
• W2154100940 hasRelatedWork W2912581653 @default.

• next