FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2050894766> ?p ?o ?g. }

• W2050894766 endingPage "108" @default.
• W2050894766 startingPage "98" @default.
• W2050894766 abstract "Abstract Cross-shore velocity profiles are measured at 0.001 m vertical resolution and at 100 Hz over the lower 0.02–0.07 m of the water column in the mid swash zone on a dissipative, macrotidal beach. Swash motion is predominantly at infragravity frequencies and forced by significant wave heights exceeding 1.5 m and peak wave periods over 15 s. Observations of long duration (> 14 s) swashes during two rising tides are used to quantify the vertical structure of cross-shore flow velocities and estimate corresponding bed shear stress and friction coefficients. Analysis is performed on an individual swash event to an elevation of 0.07 m and an ensemble event made up of 24 individual swash events to an elevation of 0.02 m. Cross-shore velocities exceed 2 m s−1 and are of a similar magnitude during both the uprush and the backwash. Changes in velocity with elevation indicate that the swash zone boundary layer extends to 0.07 m during the strongest flows and is well-represented by the logarithmic model applied to this elevation, except near flow reversal. Maximum bed shear stresses estimated using the logarithmic model are 22 N m−2 and 10 N m−2 for the individual event and ensemble event respectively and mean values are larger during the backwash than the uprush. Mean friction coefficients estimated from equating the logarithmic model and the quadratic drag law are 0.018 and 0.019 for the individual event and ensemble event respectively. Bed shear stress may be underestimated if the logarithmic model is fit to a velocity profile that is only part boundary layer, emphasising the need for high resolution velocity profiles close to the bed for accurate bed shear stress predictions in the swash zone." @default.
• W2050894766 created "2016-06-24" @default.
• W2050894766 creator A5019794595 @default.
• W2050894766 creator A5039352496 @default.
• W2050894766 creator A5043528740 @default.
• W2050894766 creator A5088603296 @default.
• W2050894766 creator A5090161001 @default.
• W2050894766 date "2015-06-01" @default.
• W2050894766 modified "2023-10-03" @default.
• W2050894766 title "Vertical structure of near-bed cross-shore flow velocities in the swash zone of a dissipative beach" @default.
• W2050894766 cites W1967694629 @default.
• W2050894766 cites W1969393339 @default.
• W2050894766 cites W1969504368 @default.
• W2050894766 cites W1971818170 @default.
• W2050894766 cites W1977275889 @default.
• W2050894766 cites W1980884881 @default.
• W2050894766 cites W1984537331 @default.
• W2050894766 cites W1988097655 @default.
• W2050894766 cites W1996774181 @default.
• W2050894766 cites W1997962158 @default.
• W2050894766 cites W1999150101 @default.
• W2050894766 cites W2005394262 @default.
• W2050894766 cites W2005690057 @default.
• W2050894766 cites W2007272193 @default.
• W2050894766 cites W2012079191 @default.
• W2050894766 cites W2015999197 @default.
• W2050894766 cites W2032600491 @default.
• W2050894766 cites W2036590641 @default.
• W2050894766 cites W2040287838 @default.
• W2050894766 cites W2042539537 @default.
• W2050894766 cites W2049092507 @default.
• W2050894766 cites W2049358280 @default.
• W2050894766 cites W2077266785 @default.
• W2050894766 cites W2077392542 @default.
• W2050894766 cites W2080019512 @default.
• W2050894766 cites W2083380664 @default.
• W2050894766 cites W2089257670 @default.
• W2050894766 cites W2115437873 @default.
• W2050894766 cites W2160903673 @default.
• W2050894766 cites W2161827836 @default.
• W2050894766 cites W2312232316 @default.
• W2050894766 doi "https://doi.org/10.1016/j.csr.2015.04.006" @default.
• W2050894766 hasPublicationYear "2015" @default.
• W2050894766 type Work @default.
• W2050894766 sameAs 2050894766 @default.
• W2050894766 citedByCount "8" @default.
• W2050894766 countsByYear W20508947662016 @default.
• W2050894766 countsByYear W20508947662017 @default.
• W2050894766 countsByYear W20508947662018 @default.
• W2050894766 countsByYear W20508947662019 @default.
• W2050894766 countsByYear W20508947662020 @default.
• W2050894766 countsByYear W20508947662021 @default.
• W2050894766 countsByYear W20508947662023 @default.
• W2050894766 crossrefType "journal-article" @default.
• W2050894766 hasAuthorship W2050894766A5019794595 @default.
• W2050894766 hasAuthorship W2050894766A5039352496 @default.
• W2050894766 hasAuthorship W2050894766A5043528740 @default.
• W2050894766 hasAuthorship W2050894766A5088603296 @default.
• W2050894766 hasAuthorship W2050894766A5090161001 @default.
• W2050894766 hasBestOaLocation W20508947662 @default.
• W2050894766 hasConcept C111368507 @default.
• W2050894766 hasConcept C114793014 @default.
• W2050894766 hasConcept C121332964 @default.
• W2050894766 hasConcept C127313418 @default.
• W2050894766 hasConcept C152382732 @default.
• W2050894766 hasConcept C187320778 @default.
• W2050894766 hasConcept C2775891797 @default.
• W2050894766 hasConcept C38349280 @default.
• W2050894766 hasConcept C57879066 @default.
• W2050894766 hasConcept C62520636 @default.
• W2050894766 hasConcept C83877588 @default.
• W2050894766 hasConcept C99692599 @default.
• W2050894766 hasConceptScore W2050894766C111368507 @default.
• W2050894766 hasConceptScore W2050894766C114793014 @default.
• W2050894766 hasConceptScore W2050894766C121332964 @default.
• W2050894766 hasConceptScore W2050894766C127313418 @default.
• W2050894766 hasConceptScore W2050894766C152382732 @default.
• W2050894766 hasConceptScore W2050894766C187320778 @default.
• W2050894766 hasConceptScore W2050894766C2775891797 @default.
• W2050894766 hasConceptScore W2050894766C38349280 @default.
• W2050894766 hasConceptScore W2050894766C57879066 @default.
• W2050894766 hasConceptScore W2050894766C62520636 @default.
• W2050894766 hasConceptScore W2050894766C83877588 @default.
• W2050894766 hasConceptScore W2050894766C99692599 @default.
• W2050894766 hasFunder F4320306076 @default.
• W2050894766 hasFunder F4320308928 @default.
• W2050894766 hasLocation W20508947661 @default.
• W2050894766 hasLocation W20508947662 @default.
• W2050894766 hasOpenAccess W2050894766 @default.
• W2050894766 hasPrimaryLocation W20508947661 @default.
• W2050894766 hasRelatedWork W1582754465 @default.
• W2050894766 hasRelatedWork W1822816900 @default.
• W2050894766 hasRelatedWork W2011543936 @default.
• W2050894766 hasRelatedWork W2062944209 @default.
• W2050894766 hasRelatedWork W2087280628 @default.
• W2050894766 hasRelatedWork W2141661912 @default.
• W2050894766 hasRelatedWork W2406769714 @default.
• W2050894766 hasRelatedWork W2886264500 @default.

• next