FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2169777983> ?p ?o ?g. }

• W2169777983 endingPage "1920" @default.
• W2169777983 startingPage "1905" @default.
• W2169777983 abstract "Abstract A 3D hydrodynamic model [Regional Ocean Model System (ROMS)] is used to investigate how axial wind influences stratification and to explore the associated longitudinal salt transport in partially mixed estuaries. The model is configured to represent a straight estuarine channel connecting to a shelf sea. The results confirm that wind straining of the along-channel salinity gradient exerts an important control on stratification. Two governing parameters are identified: the Wedderburn number (W) defined as the ratio of wind stress to axial baroclinic pressure gradient force, and the ratio of an entrainment depth to water depth (hs/H). Here W controls the effectiveness of wind straining, which promotes increases (decreases) in stratification during down-estuary (up-estuary) wind. The ratio hs/H determines the portion of the water column affected by direct wind mixing. While stratification is always reduced by up-estuary wind, stratification shows an increase-then-decrease transition when down-estuary wind stress increases. Such transition is a result of the competition between wind straining and direct wind mixing. A horizontal Richardson number modified to include wind straining/mixing is shown to reasonably represent the transition, and a regime diagram is proposed to classify the wind’s role on stratification. Mechanisms driving salt flux during axial wind events are also explored. At the onset and end of the wind events, barotropic adjustment drives strong transient salt fluxes. Net salt flux is controlled by the responses of subtidal shear dispersion to wind forcing. Moderate down-estuary winds enhance subtidal shear dispersion, whereas up-estuary winds always reduce it. Supporting observations from upper Chesapeake Bay are presented." @default.
• W2169777983 created "2016-06-24" @default.
• W2169777983 creator A5039545769 @default.
• W2169777983 creator A5086003066 @default.
• W2169777983 date "2009-08-01" @default.
• W2169777983 modified "2023-10-17" @default.
• W2169777983 title "Axial Wind Effects on Stratification and Longitudinal Salt Transport in an Idealized, Partially Mixed Estuary*" @default.
• W2169777983 cites W1966981265 @default.
• W2169777983 cites W1968913971 @default.
• W2169777983 cites W1973687127 @default.
• W2169777983 cites W1977852787 @default.
• W2169777983 cites W1979206658 @default.
• W2169777983 cites W1989282335 @default.
• W2169777983 cites W1991121489 @default.
• W2169777983 cites W1999926394 @default.
• W2169777983 cites W2002338553 @default.
• W2169777983 cites W2002627764 @default.
• W2169777983 cites W2005043675 @default.
• W2169777983 cites W2016216840 @default.
• W2169777983 cites W2018142367 @default.
• W2169777983 cites W2023281773 @default.
• W2169777983 cites W2033491954 @default.
• W2169777983 cites W2043121152 @default.
• W2169777983 cites W2051761435 @default.
• W2169777983 cites W2056266266 @default.
• W2169777983 cites W2057137472 @default.
• W2169777983 cites W2058216830 @default.
• W2169777983 cites W2063300091 @default.
• W2169777983 cites W2067808220 @default.
• W2169777983 cites W2069384562 @default.
• W2169777983 cites W2070160679 @default.
• W2169777983 cites W2071683738 @default.
• W2169777983 cites W2077391889 @default.
• W2169777983 cites W2082165664 @default.
• W2169777983 cites W2083842822 @default.
• W2169777983 cites W2084779007 @default.
• W2169777983 cites W2091455287 @default.
• W2169777983 cites W2100362728 @default.
• W2169777983 cites W2101376597 @default.
• W2169777983 cites W2103418513 @default.
• W2169777983 cites W2105799849 @default.
• W2169777983 cites W2109107114 @default.
• W2169777983 cites W2111257251 @default.
• W2169777983 cites W2119603362 @default.
• W2169777983 cites W2120828264 @default.
• W2169777983 cites W2127861825 @default.
• W2169777983 cites W2172505164 @default.
• W2169777983 cites W2175739291 @default.
• W2169777983 cites W2176346484 @default.
• W2169777983 cites W2188455334 @default.
• W2169777983 cites W2321434447 @default.
• W2169777983 cites W4244780620 @default.
• W2169777983 doi "https://doi.org/10.1175/2009jpo4016.1" @default.
• W2169777983 hasPublicationYear "2009" @default.
• W2169777983 type Work @default.
• W2169777983 sameAs 2169777983 @default.
• W2169777983 citedByCount "121" @default.
• W2169777983 countsByYear W21697779832012 @default.
• W2169777983 countsByYear W21697779832013 @default.
• W2169777983 countsByYear W21697779832014 @default.
• W2169777983 countsByYear W21697779832015 @default.
• W2169777983 countsByYear W21697779832016 @default.
• W2169777983 countsByYear W21697779832017 @default.
• W2169777983 countsByYear W21697779832018 @default.
• W2169777983 countsByYear W21697779832019 @default.
• W2169777983 countsByYear W21697779832020 @default.
• W2169777983 countsByYear W21697779832021 @default.
• W2169777983 countsByYear W21697779832022 @default.
• W2169777983 countsByYear W21697779832023 @default.
• W2169777983 crossrefType "journal-article" @default.
• W2169777983 hasAuthorship W2169777983A5039545769 @default.
• W2169777983 hasAuthorship W2169777983A5086003066 @default.
• W2169777983 hasBestOaLocation W21697779831 @default.
• W2169777983 hasConcept C100701293 @default.
• W2169777983 hasConcept C100858432 @default.
• W2169777983 hasConcept C107674354 @default.
• W2169777983 hasConcept C111368507 @default.
• W2169777983 hasConcept C122846477 @default.
• W2169777983 hasConcept C127313418 @default.
• W2169777983 hasConcept C135558025 @default.
• W2169777983 hasConcept C161067210 @default.
• W2169777983 hasConcept C192943249 @default.
• W2169777983 hasConcept C29712183 @default.
• W2169777983 hasConcept C3527866 @default.
• W2169777983 hasConcept C39432304 @default.
• W2169777983 hasConcept C53631411 @default.
• W2169777983 hasConcept C59822182 @default.
• W2169777983 hasConcept C86803240 @default.
• W2169777983 hasConcept C88160329 @default.
• W2169777983 hasConcept C88548481 @default.
• W2169777983 hasConcept C91586092 @default.
• W2169777983 hasConceptScore W2169777983C100701293 @default.
• W2169777983 hasConceptScore W2169777983C100858432 @default.
• W2169777983 hasConceptScore W2169777983C107674354 @default.
• W2169777983 hasConceptScore W2169777983C111368507 @default.
• W2169777983 hasConceptScore W2169777983C122846477 @default.
• W2169777983 hasConceptScore W2169777983C127313418 @default.
• W2169777983 hasConceptScore W2169777983C135558025 @default.

• next