FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2002602862> ?p ?o ?g. }

• W2002602862 endingPage "520" @default.
• W2002602862 startingPage "487" @default.
• W2002602862 abstract "During 1991–1994, repeated measurements of current structure and water mass properties were made in the major southern passages to the Caribbean Sea between Trinidad and Dominica. A total of 10 cruises were performed in different seasons, consisting primarily of serial station occupations in the Grenada, St Vincent, St Lucia, and Dominica Passages. This data set is by far the most comprehensive available in these passages and better determines the mean flow and range of variability than do previous studies. The flow structure in these passages is characterized by a strong and relatively stable inflow above the thermocline (approximately the upper 100 m), and a more highly variable flow regime within and below the thermocline. Typical near-surface inflow velocities in Grenada and St Vincent passages were 40–60 cm s−1, with maximum observed currents of 90 cm s−1. Frequently, counterflows were observed below this surface layer flowing out of the Caribbean, trapped to the southern side of the passages. This subsurface counterflow appeared to be strongest and most prevalent in Grenada Passage, where outflow speeds as large as 30 cm s−1 were observed. As a result, the ensemble mean sections for the three southern passages exhibit a deep inflow concentrated in the northern and central parts of the passages, and weak outflow on the southern sides. The ensemble of measurements from this program indicate a mean transport of 9.5±3 × 106 m3 s−1 through the southern passages, with a range of variability from 3 to 17 × 106 m3 s−1. No clear annual cycle is apparent in the passage transports. Mean transports calculated for the individual passages were 4.7, 3.4, 0.9, and 0.5 × 106 m3 s−1, respectively, for Grenada, St Vincent, St Lucia, and Dominica Passages, decreasing monotonically northward and indicating that Grenada and St Vincent Passages largely dominate the inflow to the southern Caribbean. Consideration of this data set, historical data, Sverdrup theory and numerical model results suggests that very little of the mean inflow to the Caribbean through the southern passages can be attributed to wind-driven circulation, and that most of the transport (6–8 × 106 m3 s−1) is derived from South Atlantic waters crossing the equator in the upper limb of the Atlantic thermohaline cell. The remainder of the upper ocean thermohaline transport likely follows a different route into the subtropical gyre, possibly flowing northward in the interior and entering the Caribbean through the more northern passages." @default.
• W2002602862 created "2016-06-24" @default.
• W2002602862 creator A5029137939 @default.
• W2002602862 creator A5062162846 @default.
• W2002602862 date "1997-03-01" @default.
• W2002602862 modified "2023-10-03" @default.
• W2002602862 title "Velocity structure and transport in the Windward Islands Passages" @default.
• W2002602862 cites W1630056199 @default.
• W2002602862 cites W1971245813 @default.
• W2002602862 cites W1976375472 @default.
• W2002602862 cites W1981669700 @default.
• W2002602862 cites W1989306712 @default.
• W2002602862 cites W1991675964 @default.
• W2002602862 cites W1995847317 @default.
• W2002602862 cites W1999598206 @default.
• W2002602862 cites W2012984343 @default.
• W2002602862 cites W2026212054 @default.
• W2002602862 cites W2035370616 @default.
• W2002602862 cites W2037832350 @default.
• W2002602862 cites W2038181778 @default.
• W2002602862 cites W2038398924 @default.
• W2002602862 cites W2048783255 @default.
• W2002602862 cites W2058464211 @default.
• W2002602862 cites W2058740921 @default.
• W2002602862 cites W2065047495 @default.
• W2002602862 cites W2075674992 @default.
• W2002602862 cites W2089969242 @default.
• W2002602862 cites W2091312895 @default.
• W2002602862 cites W2117719298 @default.
• W2002602862 cites W2119469414 @default.
• W2002602862 cites W2119797313 @default.
• W2002602862 cites W2133507371 @default.
• W2002602862 cites W2142636472 @default.
• W2002602862 cites W2174228892 @default.
• W2002602862 doi "https://doi.org/10.1016/s0967-0637(96)00113-6" @default.
• W2002602862 hasPublicationYear "1997" @default.
• W2002602862 type Work @default.
• W2002602862 sameAs 2002602862 @default.
• W2002602862 citedByCount "54" @default.
• W2002602862 countsByYear W20026028622012 @default.
• W2002602862 countsByYear W20026028622013 @default.
• W2002602862 countsByYear W20026028622014 @default.
• W2002602862 countsByYear W20026028622015 @default.
• W2002602862 countsByYear W20026028622017 @default.
• W2002602862 countsByYear W20026028622018 @default.
• W2002602862 countsByYear W20026028622020 @default.
• W2002602862 countsByYear W20026028622021 @default.
• W2002602862 countsByYear W20026028622022 @default.
• W2002602862 countsByYear W20026028622023 @default.
• W2002602862 crossrefType "journal-article" @default.
• W2002602862 hasAuthorship W2002602862A5029137939 @default.
• W2002602862 hasAuthorship W2002602862A5062162846 @default.
• W2002602862 hasBestOaLocation W20026028621 @default.
• W2002602862 hasConcept C105824904 @default.
• W2002602862 hasConcept C111368507 @default.
• W2002602862 hasConcept C121332964 @default.
• W2002602862 hasConcept C127313418 @default.
• W2002602862 hasConcept C148043351 @default.
• W2002602862 hasConcept C159985019 @default.
• W2002602862 hasConcept C192562407 @default.
• W2002602862 hasConcept C204323151 @default.
• W2002602862 hasConcept C2776132308 @default.
• W2002602862 hasConcept C38349280 @default.
• W2002602862 hasConcept C49204034 @default.
• W2002602862 hasConcept C57879066 @default.
• W2002602862 hasConcept C86132830 @default.
• W2002602862 hasConceptScore W2002602862C105824904 @default.
• W2002602862 hasConceptScore W2002602862C111368507 @default.
• W2002602862 hasConceptScore W2002602862C121332964 @default.
• W2002602862 hasConceptScore W2002602862C127313418 @default.
• W2002602862 hasConceptScore W2002602862C148043351 @default.
• W2002602862 hasConceptScore W2002602862C159985019 @default.
• W2002602862 hasConceptScore W2002602862C192562407 @default.
• W2002602862 hasConceptScore W2002602862C204323151 @default.
• W2002602862 hasConceptScore W2002602862C2776132308 @default.
• W2002602862 hasConceptScore W2002602862C38349280 @default.
• W2002602862 hasConceptScore W2002602862C49204034 @default.
• W2002602862 hasConceptScore W2002602862C57879066 @default.
• W2002602862 hasConceptScore W2002602862C86132830 @default.
• W2002602862 hasIssue "3" @default.
• W2002602862 hasLocation W20026028621 @default.
• W2002602862 hasOpenAccess W2002602862 @default.
• W2002602862 hasPrimaryLocation W20026028621 @default.
• W2002602862 hasRelatedWork W1590524616 @default.
• W2002602862 hasRelatedWork W1978892611 @default.
• W2002602862 hasRelatedWork W2002602862 @default.
• W2002602862 hasRelatedWork W2102774520 @default.
• W2002602862 hasRelatedWork W2117562840 @default.
• W2002602862 hasRelatedWork W2281531441 @default.
• W2002602862 hasRelatedWork W2746815904 @default.
• W2002602862 hasRelatedWork W3022122985 @default.
• W2002602862 hasRelatedWork W4250676245 @default.
• W2002602862 hasRelatedWork W757371169 @default.
• W2002602862 hasVolume "44" @default.
• W2002602862 isParatext "false" @default.
• W2002602862 isRetracted "false" @default.
• W2002602862 magId "2002602862" @default.
• W2002602862 workType "article" @default.