FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016364060> ?p ?o ?g. }

• W2016364060 endingPage "27884" @default.
• W2016364060 startingPage "27867" @default.
• W2016364060 abstract "Edge waves react to the presence of a mean longshore current as though the current was a change in bottom topography. In this way, the cross‐shore shape of the edge wave can be amplified over the current, relative to the shoreline, in the same way as the edge wave shape can be amplified over bars. On a beach with both longshore currents and bars, the degree of edge wave amplification (or trapping) depends on the strength and location of the longshore current shear relative to the steepness of the bottom slope and also on the direction of edge wave propagation relative to the longshore current. Weak longshore current shear over well‐developed bars does not significantly alter edge wave trapping over bars simply enhancing or reducing the existing bar trapping effect. Conversely, strong current shears over gentle topography can govern the existence and location of edge wave trapping, the extreme example being edge wave trapping on plane beaches where the amplification is entirely due to the existence of mean longshore currents. In reality the possibilities are restricted, since the shape of the longshore current profile is primarily determined by the pattern of incident wave breaking, which itself depends on the beach profile. The importance of realistic current shear relative to realistic bottom slope in determining edge wave shape is demonstrated using frequency‐wavenumber spectra taken during the Duck Experiment on Low‐Frequency and Incident‐band Longshore and Across‐shore Hydrodynamics (DELILAH) at Duck, North Carolina. These frequency‐wavenumber spectra show a general dominance of edge waves traveling with the longshore current. In cases where the current shear is strong relative to the bottom slope, the location of edge wave trapping changes as the longshore current profile changes with the tide. When the bar was well defined, the longshore current shear was rarely strong enough to influence the existence or location of edge wave trapping, but could have a enhancing effect. While past work [i.e. Schönfeldt , 1995] has suggested that edge waves, trapped and amplified on longshore currents, may cause bars to form on plane beaches and bars to move on barred beaches, these observations suggest that under most conditions, edge wave trapping on longshore currents is a subtle effect, modulated by sea level changes, and is unlikely to produce significant morphological change unless the current is very strong." @default.
• W2016364060 created "2016-06-24" @default.
• W2016364060 creator A5087107574 @default.
• W2016364060 creator A5089111680 @default.
• W2016364060 date "1998-11-15" @default.
• W2016364060 modified "2023-10-13" @default.
• W2016364060 title "Bar‐trapped edge waves and longshore currents" @default.
• W2016364060 cites W2012558930 @default.
• W2016364060 cites W2021337989 @default.
• W2016364060 cites W2027196445 @default.
• W2016364060 cites W2028207159 @default.
• W2016364060 cites W2029375677 @default.
• W2016364060 cites W2033922649 @default.
• W2016364060 cites W2049576659 @default.
• W2016364060 cites W2050225901 @default.
• W2016364060 cites W2072731583 @default.
• W2016364060 cites W2074688739 @default.
• W2016364060 cites W2078476303 @default.
• W2016364060 cites W2078778446 @default.
• W2016364060 cites W2088497439 @default.
• W2016364060 cites W2091619208 @default.
• W2016364060 cites W2094693849 @default.
• W2016364060 cites W2100949948 @default.
• W2016364060 cites W2132412827 @default.
• W2016364060 cites W2147635808 @default.
• W2016364060 cites W2169773257 @default.
• W2016364060 doi "https://doi.org/10.1029/98jc02098" @default.
• W2016364060 hasPublicationYear "1998" @default.
• W2016364060 type Work @default.
• W2016364060 sameAs 2016364060 @default.
• W2016364060 citedByCount "16" @default.
• W2016364060 countsByYear W20163640602012 @default.
• W2016364060 countsByYear W20163640602013 @default.
• W2016364060 countsByYear W20163640602015 @default.
• W2016364060 countsByYear W20163640602021 @default.
• W2016364060 crossrefType "journal-article" @default.
• W2016364060 hasAuthorship W2016364060A5087107574 @default.
• W2016364060 hasAuthorship W2016364060A5089111680 @default.
• W2016364060 hasConcept C111368507 @default.
• W2016364060 hasConcept C114793014 @default.
• W2016364060 hasConcept C120665830 @default.
• W2016364060 hasConcept C121130766 @default.
• W2016364060 hasConcept C121332964 @default.
• W2016364060 hasConcept C127313418 @default.
• W2016364060 hasConcept C148043351 @default.
• W2016364060 hasConcept C152382732 @default.
• W2016364060 hasConcept C162307627 @default.
• W2016364060 hasConcept C197631562 @default.
• W2016364060 hasConcept C2524010 @default.
• W2016364060 hasConcept C2816523 @default.
• W2016364060 hasConcept C33923547 @default.
• W2016364060 hasConcept C41008148 @default.
• W2016364060 hasConcept C5900021 @default.
• W2016364060 hasConcept C65589250 @default.
• W2016364060 hasConcept C70620910 @default.
• W2016364060 hasConcept C76155785 @default.
• W2016364060 hasConcept C8058405 @default.
• W2016364060 hasConcept C96035792 @default.
• W2016364060 hasConceptScore W2016364060C111368507 @default.
• W2016364060 hasConceptScore W2016364060C114793014 @default.
• W2016364060 hasConceptScore W2016364060C120665830 @default.
• W2016364060 hasConceptScore W2016364060C121130766 @default.
• W2016364060 hasConceptScore W2016364060C121332964 @default.
• W2016364060 hasConceptScore W2016364060C127313418 @default.
• W2016364060 hasConceptScore W2016364060C148043351 @default.
• W2016364060 hasConceptScore W2016364060C152382732 @default.
• W2016364060 hasConceptScore W2016364060C162307627 @default.
• W2016364060 hasConceptScore W2016364060C197631562 @default.
• W2016364060 hasConceptScore W2016364060C2524010 @default.
• W2016364060 hasConceptScore W2016364060C2816523 @default.
• W2016364060 hasConceptScore W2016364060C33923547 @default.
• W2016364060 hasConceptScore W2016364060C41008148 @default.
• W2016364060 hasConceptScore W2016364060C5900021 @default.
• W2016364060 hasConceptScore W2016364060C65589250 @default.
• W2016364060 hasConceptScore W2016364060C70620910 @default.
• W2016364060 hasConceptScore W2016364060C76155785 @default.
• W2016364060 hasConceptScore W2016364060C8058405 @default.
• W2016364060 hasConceptScore W2016364060C96035792 @default.
• W2016364060 hasIssue "C12" @default.
• W2016364060 hasLocation W20163640601 @default.
• W2016364060 hasOpenAccess W2016364060 @default.
• W2016364060 hasPrimaryLocation W20163640601 @default.
• W2016364060 hasRelatedWork W1506249783 @default.
• W2016364060 hasRelatedWork W1977973012 @default.
• W2016364060 hasRelatedWork W2001088508 @default.
• W2016364060 hasRelatedWork W2332152992 @default.
• W2016364060 hasRelatedWork W2886430871 @default.
• W2016364060 hasRelatedWork W2949029579 @default.
• W2016364060 hasRelatedWork W3011438701 @default.
• W2016364060 hasRelatedWork W3148450583 @default.
• W2016364060 hasRelatedWork W4238008884 @default.
• W2016364060 hasRelatedWork W4376130101 @default.
• W2016364060 hasVolume "103" @default.
• W2016364060 isParatext "false" @default.
• W2016364060 isRetracted "false" @default.
• W2016364060 magId "2016364060" @default.
• W2016364060 workType "article" @default.