FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2011134529> ?p ?o ?g. }

• W2011134529 endingPage "906" @default.
• W2011134529 startingPage "871" @default.
• W2011134529 abstract "In February 1991, an array of six current-meter moorings was deployed for one year across the central California outer shelf and slope. The main line of the array extended 30 km offshore of the shelf break, out to water depths of 1400 m. A more sparsely-instrumented line, displaced 30 km to the northwest, extended 14 km offshore. Though shorter, the northern line spanned similar water depths because the gradient of the topography steepened in the northern region. A poleward flow pattern, typical of the California undercurrent, was seen across both lines in the array over most of the year. The poleward flow was surface intensified. In general, the portion of the undercurrent that crossed the southern line had larger amplitudes and penetrated more deeply into the water column than the portion that crossed the northern line. Transport over the year ranged from 0 to 2.5 Sverdrups (Sv) poleward across the southern line; 0 to 1 Sv poleward across the northern line. We suggest the difference in transport was caused by topographic constraints, which tended to force the poleward flow offshore of the northern measurement sites. The slope of the topography steepened too abruptly to allow the poleward flow to follow isobaths when currents were strong. When current velocities lessened, a more coherent flow pattern was seen across both lines in the array. In general, the poleward flow patterns in the undercurrent were not affected by local winds or by the local alongshore pressure gradient. Nor was a strong seasonal pattern evident. Rather unexpectedly, a small but statistically significant fraction of the current variance over the mid- and outer slope was driven by the surface wind stress. An alongshelf wind stress caused currents to flow along the slope, parallel to the wind field, down to depths of 400 m below the surface and out to distances of 2 Rossby radii past the shelf break. The transfer functions were weak, 3–4 cm/s per dyn cm−2, but comparable to wind-driven current amplitudes of 4–6 cm/s per unit wind stress over the middle shelf. Equatorward, alongshelf winds also caused water from 200–300 m over the slope to upwell onto the shelf as the surface water moved offshore." @default.
• W2011134529 created "2016-06-24" @default.
• W2011134529 creator A5033390004 @default.
• W2011134529 creator A5040708637 @default.
• W2011134529 date "2000-05-01" @default.
• W2011134529 modified "2023-10-16" @default.
• W2011134529 title "Subtidal currents over the central California slope: evidence for offshore veering of the undercurrent and for direct, wind-driven slope currents" @default.
• W2011134529 cites W1966727937 @default.
• W2011134529 cites W1990480127 @default.
• W2011134529 cites W1997186446 @default.
• W2011134529 cites W1998036329 @default.
• W2011134529 cites W2008891710 @default.
• W2011134529 cites W2011064489 @default.
• W2011134529 cites W2016345318 @default.
• W2011134529 cites W2038392936 @default.
• W2011134529 cites W2042181630 @default.
• W2011134529 cites W2042453801 @default.
• W2011134529 cites W2044409970 @default.
• W2011134529 cites W2046153412 @default.
• W2011134529 cites W2048316209 @default.
• W2011134529 cites W2056947354 @default.
• W2011134529 cites W2065333897 @default.
• W2011134529 cites W2074158810 @default.
• W2011134529 cites W2074589901 @default.
• W2011134529 cites W2075967820 @default.
• W2011134529 cites W2092973916 @default.
• W2011134529 cites W2127274451 @default.
• W2011134529 cites W2127736339 @default.
• W2011134529 cites W2143347680 @default.
• W2011134529 cites W2153599305 @default.
• W2011134529 cites W2162024977 @default.
• W2011134529 cites W2169564961 @default.
• W2011134529 cites W2174120788 @default.
• W2011134529 cites W2179948352 @default.
• W2011134529 cites W2263908194 @default.
• W2011134529 cites W72055766 @default.
• W2011134529 doi "https://doi.org/10.1016/s0967-0645(99)00130-7" @default.
• W2011134529 hasPublicationYear "2000" @default.
• W2011134529 type Work @default.
• W2011134529 sameAs 2011134529 @default.
• W2011134529 citedByCount "36" @default.
• W2011134529 countsByYear W20111345292012 @default.
• W2011134529 countsByYear W20111345292013 @default.
• W2011134529 countsByYear W20111345292014 @default.
• W2011134529 countsByYear W20111345292015 @default.
• W2011134529 countsByYear W20111345292016 @default.
• W2011134529 countsByYear W20111345292017 @default.
• W2011134529 countsByYear W20111345292018 @default.
• W2011134529 countsByYear W20111345292020 @default.
• W2011134529 countsByYear W20111345292021 @default.
• W2011134529 countsByYear W20111345292023 @default.
• W2011134529 crossrefType "journal-article" @default.
• W2011134529 hasAuthorship W2011134529A5033390004 @default.
• W2011134529 hasAuthorship W2011134529A5040708637 @default.
• W2011134529 hasConcept C111368507 @default.
• W2011134529 hasConcept C127313418 @default.
• W2011134529 hasConcept C148043351 @default.
• W2011134529 hasConcept C162284963 @default.
• W2011134529 hasConcept C184751465 @default.
• W2011134529 hasConcept C198352243 @default.
• W2011134529 hasConcept C2524010 @default.
• W2011134529 hasConcept C33923547 @default.
• W2011134529 hasConcept C38349280 @default.
• W2011134529 hasConcept C52526452 @default.
• W2011134529 hasConcept C98156149 @default.
• W2011134529 hasConceptScore W2011134529C111368507 @default.
• W2011134529 hasConceptScore W2011134529C127313418 @default.
• W2011134529 hasConceptScore W2011134529C148043351 @default.
• W2011134529 hasConceptScore W2011134529C162284963 @default.
• W2011134529 hasConceptScore W2011134529C184751465 @default.
• W2011134529 hasConceptScore W2011134529C198352243 @default.
• W2011134529 hasConceptScore W2011134529C2524010 @default.
• W2011134529 hasConceptScore W2011134529C33923547 @default.
• W2011134529 hasConceptScore W2011134529C38349280 @default.
• W2011134529 hasConceptScore W2011134529C52526452 @default.
• W2011134529 hasConceptScore W2011134529C98156149 @default.
• W2011134529 hasIssue "5-6" @default.
• W2011134529 hasLocation W20111345291 @default.
• W2011134529 hasOpenAccess W2011134529 @default.
• W2011134529 hasPrimaryLocation W20111345291 @default.
• W2011134529 hasRelatedWork W1862660820 @default.
• W2011134529 hasRelatedWork W1979235997 @default.
• W2011134529 hasRelatedWork W2948072715 @default.
• W2011134529 hasRelatedWork W3008642600 @default.
• W2011134529 hasRelatedWork W3101236539 @default.
• W2011134529 hasRelatedWork W3106924474 @default.
• W2011134529 hasRelatedWork W3109095322 @default.
• W2011134529 hasRelatedWork W3110144435 @default.
• W2011134529 hasRelatedWork W834248173 @default.
• W2011134529 hasRelatedWork W3110323075 @default.
• W2011134529 hasVolume "47" @default.
• W2011134529 isParatext "false" @default.
• W2011134529 isRetracted "false" @default.
• W2011134529 magId "2011134529" @default.
• W2011134529 workType "article" @default.