FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2144185364> ?p ?o ?g. }

• W2144185364 endingPage "1904" @default.
• W2144185364 startingPage "1884" @default.
• W2144185364 abstract "High frequency (HF) radar surface velocities and coastal tidal gauge data are assimilated into a two-dimensional (2D) finite element spectral in time model to describe the Stokes drift of the major tidal constituents in the English Channel. The numerical model was fit to observations by optimizing the unknown sea surface height at the open boundaries of the domain. Six major tidal constituents, M2, S2, N2, K2, K1, and M4 were subject to the inversion. The assimilated sea surface height and depth averaged velocities are used for mapping of the residual transport through the Channel, tidal dissipation, and for estimation of the energy flux. The respective values obtained are 53±6×103 m3 s−1 for the net combined transport of the residual flow, and 0.75±0.16 W m−2, for the basin-averaged tidal energy dissipation rate. The net horizontal energy flux through the Dover Strait is estimated as 1.40±0.16×1010 W. Analysis of the stream function distribution of the residual flow reveals a number of permanent eddies associated with peculiarities of the coastline shape and inhomogeneities of the bottom topography. We perform an extensive error analysis of the results via an explicit inversion of the Hessian matrix, associated with the assimilation scheme. Error charts for the sea surface elevation demonstrate the model's ability to fit the data within the error bars in the major part of the model domain and expose coastal areas within the western Channel requiring better coverage by observations." @default.
• W2144185364 created "2016-06-24" @default.
• W2144185364 creator A5026213794 @default.
• W2144185364 creator A5066225248 @default.
• W2144185364 creator A5079646637 @default.
• W2144185364 date "2006-10-01" @default.
• W2144185364 modified "2023-10-14" @default.
• W2144185364 title "Residual circulation in the English Channel as a dynamically consistent synthesis of shore-based observations of sea level and currents" @default.
• W2144185364 cites W1976310296 @default.
• W2144185364 cites W1984058915 @default.
• W2144185364 cites W1984121505 @default.
• W2144185364 cites W1989422506 @default.
• W2144185364 cites W1992650170 @default.
• W2144185364 cites W2013418882 @default.
• W2144185364 cites W2016006371 @default.
• W2144185364 cites W2016329289 @default.
• W2144185364 cites W2019124538 @default.
• W2144185364 cites W2025865840 @default.
• W2144185364 cites W2027837831 @default.
• W2144185364 cites W2028486576 @default.
• W2144185364 cites W2037999582 @default.
• W2144185364 cites W2038523482 @default.
• W2144185364 cites W2042121449 @default.
• W2144185364 cites W2054225964 @default.
• W2144185364 cites W2074353255 @default.
• W2144185364 cites W2076843499 @default.
• W2144185364 cites W2113927532 @default.
• W2144185364 cites W2123774837 @default.
• W2144185364 cites W2129141859 @default.
• W2144185364 cites W2130844535 @default.
• W2144185364 cites W2146876467 @default.
• W2144185364 cites W2169555346 @default.
• W2144185364 cites W2177073435 @default.
• W2144185364 cites W2177999089 @default.
• W2144185364 cites W2179442574 @default.
• W2144185364 doi "https://doi.org/10.1016/j.csr.2006.06.006" @default.
• W2144185364 hasPublicationYear "2006" @default.
• W2144185364 type Work @default.
• W2144185364 sameAs 2144185364 @default.
• W2144185364 citedByCount "15" @default.
• W2144185364 countsByYear W21441853642012 @default.
• W2144185364 countsByYear W21441853642013 @default.
• W2144185364 countsByYear W21441853642015 @default.
• W2144185364 countsByYear W21441853642016 @default.
• W2144185364 countsByYear W21441853642019 @default.
• W2144185364 countsByYear W21441853642023 @default.
• W2144185364 crossrefType "journal-article" @default.
• W2144185364 hasAuthorship W2144185364A5026213794 @default.
• W2144185364 hasAuthorship W2144185364A5066225248 @default.
• W2144185364 hasAuthorship W2144185364A5079646637 @default.
• W2144185364 hasConcept C11413529 @default.
• W2144185364 hasConcept C121332964 @default.
• W2144185364 hasConcept C127313418 @default.
• W2144185364 hasConcept C13280743 @default.
• W2144185364 hasConcept C135402231 @default.
• W2144185364 hasConcept C153294291 @default.
• W2144185364 hasConcept C155512373 @default.
• W2144185364 hasConcept C179065325 @default.
• W2144185364 hasConcept C196558001 @default.
• W2144185364 hasConcept C33923547 @default.
• W2144185364 hasConcept C97355855 @default.
• W2144185364 hasConceptScore W2144185364C11413529 @default.
• W2144185364 hasConceptScore W2144185364C121332964 @default.
• W2144185364 hasConceptScore W2144185364C127313418 @default.
• W2144185364 hasConceptScore W2144185364C13280743 @default.
• W2144185364 hasConceptScore W2144185364C135402231 @default.
• W2144185364 hasConceptScore W2144185364C153294291 @default.
• W2144185364 hasConceptScore W2144185364C155512373 @default.
• W2144185364 hasConceptScore W2144185364C179065325 @default.
• W2144185364 hasConceptScore W2144185364C196558001 @default.
• W2144185364 hasConceptScore W2144185364C33923547 @default.
• W2144185364 hasConceptScore W2144185364C97355855 @default.
• W2144185364 hasIssue "16" @default.
• W2144185364 hasLocation W21441853641 @default.
• W2144185364 hasLocation W21441853642 @default.
• W2144185364 hasLocation W21441853643 @default.
• W2144185364 hasOpenAccess W2144185364 @default.
• W2144185364 hasPrimaryLocation W21441853641 @default.
• W2144185364 hasRelatedWork W2045317988 @default.
• W2144185364 hasRelatedWork W2072653157 @default.
• W2144185364 hasRelatedWork W2079984045 @default.
• W2144185364 hasRelatedWork W2316789606 @default.
• W2144185364 hasRelatedWork W2347486132 @default.
• W2144185364 hasRelatedWork W2350340797 @default.
• W2144185364 hasRelatedWork W3163450759 @default.
• W2144185364 hasRelatedWork W3176908206 @default.
• W2144185364 hasRelatedWork W4293224283 @default.
• W2144185364 hasRelatedWork W4321490030 @default.
• W2144185364 hasVolume "26" @default.
• W2144185364 isParatext "false" @default.
• W2144185364 isRetracted "false" @default.
• W2144185364 magId "2144185364" @default.
• W2144185364 workType "article" @default.