FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1978759284> ?p ?o ?g. }

• W1978759284 endingPage "1247" @default.
• W1978759284 startingPage "1227" @default.
• W1978759284 abstract "Satellite-derived sea-surface temperature, TOPEX/POSEIDON (T/P) sea-level anomalies (SLAs), model wind data, and hydrographic data are used to characterize the upwelling along the Oman coast during the US Joint Global Ocean Flux Study (US JGOFS) Arabian Sea Process Study (ASPS) in 1995 as well as to look at interannual variability in the upwelling over the period 1993–1995. Empirical orthogonal function (EOF) analysis of the satellite-derived sea-surface temperature (SST) at the locations of the US JGOFS standard stations shows the first mode, which represents a biannual variability, contributes 67% of the total variance. In addition, the SST shows the upwelling “front” moving offshore with the development of Southwest (SW) Monsoon in early June 1995, reaching a maximum distance of approximately 120 km by late August 1995. Finally, SST shows the persistence of cold upwelling waters for nearly a month after the end of the SW Monsoon within the bays along the Oman coast. TOPEX/POSEIDON SLAs indicate that with the onset of the SW Monsoon, a 30-cm drop in steric height is observed along the Oman coast associated the presence of the cool upwelled waters. This drop in steric height sets up a horizontal pressure gradient and results in a compensating along-shore, northeastward-flowing, geostrophic current (East Arabian Current; EAC) during the SW Monsoon. Similarly, the altimeter data slow an offshore decrease in steric height during the Northeast (NE) Monsoon, indicating a seasonal reversal in direction of the EAC with flow to the southwest. Subsurface temperature data indicate that the actual uplifting of isotherms associated with the upwelling can be found to a distance of approximately 260 km from the shore and to a depth of 150–200 m. Using along-track altimetry data, we estimate that, for a region 260 km in offshore distance and 600 km alongshore, 2.2×106, 1.4×106 and 0.55×106 m3 s−1 were upwelled through the 100 m level with upwelling velocities O (2.0×10−5 m s−1), during the SW Monsoons of 1993, 1994 and 1995, respectively. The reduced upwelling in the summer of 1995 is attributed to a reduction in wind-stress curl along the Arabian coast when compared to 1993 and 1994." @default.
• W1978759284 created "2016-06-24" @default.
• W1978759284 creator A5037562394 @default.
• W1978759284 creator A5060995974 @default.
• W1978759284 creator A5067651225 @default.
• W1978759284 creator A5075906861 @default.
• W1978759284 date "2000-01-01" @default.
• W1978759284 modified "2023-10-17" @default.
• W1978759284 title "The Oman upwelling zone during 1993, 1994 and 1995" @default.
• W1978759284 cites W1966605412 @default.
• W1978759284 cites W1978263143 @default.
• W1978759284 cites W2011053697 @default.
• W1978759284 cites W2029554550 @default.
• W1978759284 cites W2035640345 @default.
• W1978759284 cites W2039743606 @default.
• W1978759284 cites W2053494096 @default.
• W1978759284 cites W2069156503 @default.
• W1978759284 cites W2069966948 @default.
• W1978759284 cites W2073501126 @default.
• W1978759284 cites W2077820350 @default.
• W1978759284 cites W2084927767 @default.
• W1978759284 cites W2086933696 @default.
• W1978759284 cites W2099319501 @default.
• W1978759284 cites W2113521146 @default.
• W1978759284 cites W2148879597 @default.
• W1978759284 cites W2179567393 @default.
• W1978759284 doi "https://doi.org/10.1016/s0967-0645(99)00142-3" @default.
• W1978759284 hasPublicationYear "2000" @default.
• W1978759284 type Work @default.
• W1978759284 sameAs 1978759284 @default.
• W1978759284 citedByCount "63" @default.
• W1978759284 countsByYear W19787592842012 @default.
• W1978759284 countsByYear W19787592842013 @default.
• W1978759284 countsByYear W19787592842014 @default.
• W1978759284 countsByYear W19787592842015 @default.
• W1978759284 countsByYear W19787592842016 @default.
• W1978759284 countsByYear W19787592842017 @default.
• W1978759284 countsByYear W19787592842018 @default.
• W1978759284 countsByYear W19787592842019 @default.
• W1978759284 countsByYear W19787592842020 @default.
• W1978759284 countsByYear W19787592842021 @default.
• W1978759284 countsByYear W19787592842022 @default.
• W1978759284 countsByYear W19787592842023 @default.
• W1978759284 crossrefType "journal-article" @default.
• W1978759284 hasAuthorship W1978759284A5037562394 @default.
• W1978759284 hasAuthorship W1978759284A5060995974 @default.
• W1978759284 hasAuthorship W1978759284A5067651225 @default.
• W1978759284 hasAuthorship W1978759284A5075906861 @default.
• W1978759284 hasConcept C111368507 @default.
• W1978759284 hasConcept C127313418 @default.
• W1978759284 hasConcept C13280743 @default.
• W1978759284 hasConcept C134097258 @default.
• W1978759284 hasConcept C136996986 @default.
• W1978759284 hasConcept C13724139 @default.
• W1978759284 hasConcept C142672198 @default.
• W1978759284 hasConcept C149348798 @default.
• W1978759284 hasConcept C162284963 @default.
• W1978759284 hasConcept C17534553 @default.
• W1978759284 hasConcept C39432304 @default.
• W1978759284 hasConcept C49204034 @default.
• W1978759284 hasConcept C76256466 @default.
• W1978759284 hasConcept C77942228 @default.
• W1978759284 hasConceptScore W1978759284C111368507 @default.
• W1978759284 hasConceptScore W1978759284C127313418 @default.
• W1978759284 hasConceptScore W1978759284C13280743 @default.
• W1978759284 hasConceptScore W1978759284C134097258 @default.
• W1978759284 hasConceptScore W1978759284C136996986 @default.
• W1978759284 hasConceptScore W1978759284C13724139 @default.
• W1978759284 hasConceptScore W1978759284C142672198 @default.
• W1978759284 hasConceptScore W1978759284C149348798 @default.
• W1978759284 hasConceptScore W1978759284C162284963 @default.
• W1978759284 hasConceptScore W1978759284C17534553 @default.
• W1978759284 hasConceptScore W1978759284C39432304 @default.
• W1978759284 hasConceptScore W1978759284C49204034 @default.
• W1978759284 hasConceptScore W1978759284C76256466 @default.
• W1978759284 hasConceptScore W1978759284C77942228 @default.
• W1978759284 hasIssue "7-8" @default.
• W1978759284 hasLocation W19787592841 @default.
• W1978759284 hasOpenAccess W1978759284 @default.
• W1978759284 hasPrimaryLocation W19787592841 @default.
• W1978759284 hasRelatedWork W150848716 @default.
• W1978759284 hasRelatedWork W1978759284 @default.
• W1978759284 hasRelatedWork W2031211820 @default.
• W1978759284 hasRelatedWork W2037005253 @default.
• W1978759284 hasRelatedWork W2038765681 @default.
• W1978759284 hasRelatedWork W2092973916 @default.
• W1978759284 hasRelatedWork W2396944252 @default.
• W1978759284 hasRelatedWork W255448498 @default.
• W1978759284 hasRelatedWork W2607249239 @default.
• W1978759284 hasRelatedWork W2891565871 @default.
• W1978759284 hasVolume "47" @default.
• W1978759284 isParatext "false" @default.
• W1978759284 isRetracted "false" @default.
• W1978759284 magId "1978759284" @default.
• W1978759284 workType "article" @default.