FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3161482009> ?p ?o ?g. }

• W3161482009 abstract "Abstract Rip currents are generated by surfzone wave breaking and are ejected offshore inducing inner-shelf flow spatial variability (eddies). However, surfzone effects on the inner-shelf flow spatial variability have not been studied in realistic models that include both shelf and surfzone processes. Here, these effects are diagnosed with two nearly identical twin realistic simulations of the San Diego Bight over summer to fall where one simulation includes surface gravity waves (WW) and the other that does not (NW). The simulations include tides, weak to moderate winds, internal waves, submesoscale processes, and have surfzone width L sz of 96(±41) m (≈ 1 m significant wave height). Flow spatial variability metrics, alongshore root mean square vorticity, divergence, and eddy cross-shore velocity, are analyzed in a L sz normalized cross-shore coordinate. At the surface, the metrics are consistently (> 70%) elevated in the WW run relative to NW out to 5 L sz offshore. At 4 L sz offshore, WW metrics are enhanced over the entire water column. In a fixed coordinate appropriate for eddy transport, the eddy cross-shore velocity squared correlation betweenWWand NW runs is < 0.5 out to 1.2 km offshore or 12 time-averaged L sz . The results indicate that the eddy tracer ( e.g. , larvae) transport and dispersion across the inner-shelf will be significantly different in the WW and NW runs. The WW model neglects specific surfzone vorticity generation mechanisms. Thus, these inner-shelf impacts are likely underestimated. In other regions with larger waves, impacts will extend farther offshore." @default.
• W3161482009 created "2021-05-24" @default.
• W3161482009 creator A5043762845 @default.
• W3161482009 creator A5052558370 @default.
• W3161482009 creator A5060373893 @default.
• W3161482009 date "2021-05-13" @default.
• W3161482009 modified "2023-10-17" @default.
• W3161482009 title "Diagnosing surfzone impacts on inner-shelf flow spatial variability using realistic model experiments with and without surface gravity waves" @default.
• W3161482009 cites W1507184171 @default.
• W3161482009 cites W1530345936 @default.
• W3161482009 cites W1843121426 @default.
• W3161482009 cites W1928490624 @default.
• W3161482009 cites W1979907769 @default.
• W3161482009 cites W1986738923 @default.
• W3161482009 cites W1995247297 @default.
• W3161482009 cites W2006540505 @default.
• W3161482009 cites W2007551469 @default.
• W3161482009 cites W2009195332 @default.
• W3161482009 cites W2010039478 @default.
• W3161482009 cites W2014818657 @default.
• W3161482009 cites W2029917001 @default.
• W3161482009 cites W2036747197 @default.
• W3161482009 cites W2040910310 @default.
• W3161482009 cites W2058193124 @default.
• W3161482009 cites W2063036572 @default.
• W3161482009 cites W2064520371 @default.
• W3161482009 cites W2072530451 @default.
• W3161482009 cites W2077092197 @default.
• W3161482009 cites W2087170724 @default.
• W3161482009 cites W2097481426 @default.
• W3161482009 cites W2100986500 @default.
• W3161482009 cites W2102385461 @default.
• W3161482009 cites W2109426436 @default.
• W3161482009 cites W2113548869 @default.
• W3161482009 cites W2115635295 @default.
• W3161482009 cites W2117602483 @default.
• W3161482009 cites W2119452284 @default.
• W3161482009 cites W2122557005 @default.
• W3161482009 cites W2123215027 @default.
• W3161482009 cites W2124749811 @default.
• W3161482009 cites W2127161213 @default.
• W3161482009 cites W2127993657 @default.
• W3161482009 cites W2130953273 @default.
• W3161482009 cites W2131611411 @default.
• W3161482009 cites W2133964117 @default.
• W3161482009 cites W2134607154 @default.
• W3161482009 cites W2154868214 @default.
• W3161482009 cites W2161747954 @default.
• W3161482009 cites W2163335637 @default.
• W3161482009 cites W2169339709 @default.
• W3161482009 cites W2173990665 @default.
• W3161482009 cites W2193305463 @default.
• W3161482009 cites W2228787772 @default.
• W3161482009 cites W2410152263 @default.
• W3161482009 cites W2462285898 @default.
• W3161482009 cites W2560501434 @default.
• W3161482009 cites W2595454688 @default.
• W3161482009 cites W2602525480 @default.
• W3161482009 cites W2733251851 @default.
• W3161482009 cites W2764283421 @default.
• W3161482009 cites W2784675803 @default.
• W3161482009 cites W2795357743 @default.
• W3161482009 cites W2901843809 @default.
• W3161482009 cites W2913374520 @default.
• W3161482009 cites W2958050787 @default.
• W3161482009 cites W2959826746 @default.
• W3161482009 cites W2973705640 @default.
• W3161482009 cites W2982280189 @default.
• W3161482009 cites W2990382961 @default.
• W3161482009 cites W3019871928 @default.
• W3161482009 cites W3020126810 @default.
• W3161482009 cites W3024160336 @default.
• W3161482009 cites W3116737811 @default.
• W3161482009 cites W3139042187 @default.
• W3161482009 cites W3154655306 @default.
• W3161482009 cites W3159528207 @default.
• W3161482009 doi "https://doi.org/10.1175/jpo-d-20-0324.1" @default.
• W3161482009 hasPublicationYear "2021" @default.
• W3161482009 type Work @default.
• W3161482009 sameAs 3161482009 @default.
• W3161482009 citedByCount "5" @default.
• W3161482009 countsByYear W31614820092021 @default.
• W3161482009 countsByYear W31614820092022 @default.
• W3161482009 countsByYear W31614820092023 @default.
• W3161482009 crossrefType "journal-article" @default.
• W3161482009 hasAuthorship W3161482009A5043762845 @default.
• W3161482009 hasAuthorship W3161482009A5052558370 @default.
• W3161482009 hasAuthorship W3161482009A5060373893 @default.
• W3161482009 hasBestOaLocation W31614820091 @default.
• W3161482009 hasConcept C111368507 @default.
• W3161482009 hasConcept C120665830 @default.
• W3161482009 hasConcept C121332964 @default.
• W3161482009 hasConcept C127313418 @default.
• W3161482009 hasConcept C140820882 @default.
• W3161482009 hasConcept C152382732 @default.
• W3161482009 hasConcept C153294291 @default.
• W3161482009 hasConcept C157331469 @default.
• W3161482009 hasConcept C162284963 @default.
• W3161482009 hasConcept C177562468 @default.
• W3161482009 hasConcept C179065325 @default.

• next