FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2079164804> ?p ?o ?g. }

• W2079164804 endingPage "358" @default.
• W2079164804 startingPage "323" @default.
• W2079164804 abstract "An integrated study using moored current meters, transmissometers and sediment traps revealed that sediment in Baltimore Canyon was resuspended regularly when energy from internal tides was focused along the canyon axis. Such focusing occurred primarily during late winter and early spring. During resuspension events particle concentrations at 275 m in the canyon axis typically increased from a background level of 100 μg l−1 to over 1000 μg l−1 within a 5-min period and often exceeded 5000 μg l−1. Net transport of both water and sediment 5 m above bottom (mab) at 275 m in the canyon axis was consistently downcanyon, while 5 mab at 600 m in the canyon axis net transport was upcanyon, implying convergence between the two sites. The distribution of suspended sediment was determined using a CTD/transmissometer during hydrographic transects along the canyon axis and across the slope adjacent to either side of the canyon. Resuspension on the shelf, canyon walls, and along the slope was minimal, but in the canyon interleaving tongues of turbid water were always present between 200 and 800 m. Although concentrations of resuspended sediment were high, they were not sufficient to generate downcanyon flows. Turbid plumes moved seaward along density surfaces at the convergence between 275 and 600 m and other regions of the canyon. The passage of atmospheric storms and Gulf Stream rings may have changed the pattern of currents of resuspension in portions of the canyon sometimes, but not always. Fluxes of particles collected in sediment traps along the canyon axis increased exponentially toward the buttom, but the size of particles collected in traps decreased with distance from the canyon head, suggesting that resuspended sediment was advected, but depleted in larger, denser particles away from the canyon. An exponential increase with depth in trap fluxes at 1000 m, despite fairly uniform concentrations of suspended particles measured by transmissometers, suggests that many particles are advected as large aggregates (marine snow) that are not detected quantitatively by transmissometers. Currents outside the canyon walls quickly dilute and dissipate sediment moving out of the canyon. Subamrine canyons can act as conduits of sediment to the deep ocean not only by channeling turbidity currents, but also by focusing internal tides that resuspended sediment, after which it is advected to deeper water." @default.
• W2079164804 created "2016-06-24" @default.
• W2079164804 creator A5047427383 @default.
• W2079164804 date "1989-03-01" @default.
• W2079164804 modified "2023-09-27" @default.
• W2079164804 title "Baltimore Canyon as a modern conduit of sediment to the deep sea" @default.
• W2079164804 cites W1965691397 @default.
• W2079164804 cites W1969003343 @default.
• W2079164804 cites W1973566304 @default.
• W2079164804 cites W1985121885 @default.
• W2079164804 cites W1990706702 @default.
• W2079164804 cites W2007835197 @default.
• W2079164804 cites W2014582580 @default.
• W2079164804 cites W2024274899 @default.
• W2079164804 cites W2025087013 @default.
• W2079164804 cites W2025507953 @default.
• W2079164804 cites W2026270543 @default.
• W2079164804 cites W2027797921 @default.
• W2079164804 cites W2034427910 @default.
• W2079164804 cites W2038193401 @default.
• W2079164804 cites W2042427392 @default.
• W2079164804 cites W2043899782 @default.
• W2079164804 cites W2050223194 @default.
• W2079164804 cites W2058790208 @default.
• W2079164804 cites W2062458666 @default.
• W2079164804 cites W2062490709 @default.
• W2079164804 cites W2063495438 @default.
• W2079164804 cites W2077116273 @default.
• W2079164804 cites W2085071689 @default.
• W2079164804 cites W2086784422 @default.
• W2079164804 cites W2094162551 @default.
• W2079164804 cites W2096283673 @default.
• W2079164804 cites W2130326438 @default.
• W2079164804 cites W2132832763 @default.
• W2079164804 cites W2146261730 @default.
• W2079164804 cites W2158343579 @default.
• W2079164804 doi "https://doi.org/10.1016/0198-0149(89)90041-1" @default.
• W2079164804 hasPublicationYear "1989" @default.
• W2079164804 type Work @default.
• W2079164804 sameAs 2079164804 @default.
• W2079164804 citedByCount "193" @default.
• W2079164804 countsByYear W20791648042012 @default.
• W2079164804 countsByYear W20791648042013 @default.
• W2079164804 countsByYear W20791648042014 @default.
• W2079164804 countsByYear W20791648042015 @default.
• W2079164804 countsByYear W20791648042016 @default.
• W2079164804 countsByYear W20791648042017 @default.
• W2079164804 countsByYear W20791648042018 @default.
• W2079164804 countsByYear W20791648042019 @default.
• W2079164804 countsByYear W20791648042020 @default.
• W2079164804 countsByYear W20791648042021 @default.
• W2079164804 countsByYear W20791648042022 @default.
• W2079164804 countsByYear W20791648042023 @default.
• W2079164804 crossrefType "journal-article" @default.
• W2079164804 hasAuthorship W2079164804A5047427383 @default.
• W2079164804 hasConcept C111368507 @default.
• W2079164804 hasConcept C114793014 @default.
• W2079164804 hasConcept C127313418 @default.
• W2079164804 hasConcept C187320778 @default.
• W2079164804 hasConcept C190618007 @default.
• W2079164804 hasConcept C2816523 @default.
• W2079164804 hasConcept C65589250 @default.
• W2079164804 hasConcept C69661492 @default.
• W2079164804 hasConcept C76886044 @default.
• W2079164804 hasConcept C84859931 @default.
• W2079164804 hasConceptScore W2079164804C111368507 @default.
• W2079164804 hasConceptScore W2079164804C114793014 @default.
• W2079164804 hasConceptScore W2079164804C127313418 @default.
• W2079164804 hasConceptScore W2079164804C187320778 @default.
• W2079164804 hasConceptScore W2079164804C190618007 @default.
• W2079164804 hasConceptScore W2079164804C2816523 @default.
• W2079164804 hasConceptScore W2079164804C65589250 @default.
• W2079164804 hasConceptScore W2079164804C69661492 @default.
• W2079164804 hasConceptScore W2079164804C76886044 @default.
• W2079164804 hasConceptScore W2079164804C84859931 @default.
• W2079164804 hasIssue "3" @default.
• W2079164804 hasLocation W20791648041 @default.
• W2079164804 hasOpenAccess W2079164804 @default.
• W2079164804 hasPrimaryLocation W20791648041 @default.
• W2079164804 hasRelatedWork W1542615820 @default.
• W2079164804 hasRelatedWork W1986132337 @default.
• W2079164804 hasRelatedWork W2022952157 @default.
• W2079164804 hasRelatedWork W2030675100 @default.
• W2079164804 hasRelatedWork W2086792429 @default.
• W2079164804 hasRelatedWork W2118206752 @default.
• W2079164804 hasRelatedWork W2132224644 @default.
• W2079164804 hasRelatedWork W2159045628 @default.
• W2079164804 hasRelatedWork W2616860398 @default.
• W2079164804 hasRelatedWork W3009513414 @default.
• W2079164804 hasVolume "36" @default.
• W2079164804 isParatext "false" @default.
• W2079164804 isRetracted "false" @default.
• W2079164804 magId "2079164804" @default.
• W2079164804 workType "article" @default.