FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W16282495> ?p ?o ?g. }

• W16282495 endingPage "27" @default.
• W16282495 startingPage "1" @default.
• W16282495 abstract "The principal components of the surface current system in the tropical Atlantic are the westward South Equatorial Current south of 3°N, the eastward Equatorial Countercurrent between 3°N and 10°N and the westward North Equatorial Current north of 10°N. The subsurface, eastward Equatorial Undercurrent is confined to about 1 1/2° latitude and is centered on the equator. These mean currents are subject to fluctuations over a spectrum of frequencies. Very high-frequency, turbulent fluctuations are of major importance in the mixed layers at the ocean surface and below the core of the Undercurrent. One-dimensional models cannot simulate these mixed layers because they are strongly influenced by the divergence of large-scale currents. Fluctuations with periods less than the inertial period correspond to inertia-gravity waves but their spectral properties, near 8° N, are unusual in two respects: at periods between 1/2 hr and 10 min there are very energetic oscillations associated with a thermodine-trapped internal mode; amplitudes of inertial waves below the thermodine are correlated with the intensity of surface winds. Near 5°N the inertial peak in the spectrum disappears and equator ward of 5 latitude equatorially trapped waves dominate the spectrum at periods longer than 10 days. There are hints that wave-like fluctuations do not have a universal spectrum in low latitudes. Particularly energetic equatorial oscillations observed during GATE included the following: 3-to 5-day equatorially trapped inertia-gravity waves which were forced by atmospheric disturbances with the same period; 16-day meanders of the Equatorial Undercurrent which may be related to atmospheric fluctuations with the same period; 30-day, 1000 km waves which appear to be due to instabilities of the surface currents. Superimposed on these oscillations is a trend that is part of the seasonal cycle: for example, the zonal pressure gradient in the equatorial plane increased throughout GATE, practically in phase with the intensification of the tradewinds. This information sheds light on the seasonal upwelling in the Gulf of Guinea which is not correlated with changes in the local winds." @default.
• W16282495 created "2016-06-24" @default.
• W16282495 creator A5032614869 @default.
• W16282495 creator A5083778726 @default.
• W16282495 date "1980-01-01" @default.
• W16282495 modified "2023-09-23" @default.
• W16282495 title "THE OCEANIC CIRCULATION OF THE TROPICAL ATLANTIC, AND ITS VARIABILITY, AS OBSERVED DURING GATE" @default.
• W16282495 cites W115744937 @default.
• W16282495 cites W126534596 @default.
• W16282495 cites W13898892 @default.
• W16282495 cites W1488878721 @default.
• W16282495 cites W149105755 @default.
• W16282495 cites W1977569626 @default.
• W16282495 cites W1984409652 @default.
• W16282495 cites W1985437019 @default.
• W16282495 cites W1998203115 @default.
• W16282495 cites W1998798132 @default.
• W16282495 cites W2005943898 @default.
• W16282495 cites W2008309616 @default.
• W16282495 cites W2016689653 @default.
• W16282495 cites W2023613706 @default.
• W16282495 cites W2030779692 @default.
• W16282495 cites W2035455696 @default.
• W16282495 cites W2042196073 @default.
• W16282495 cites W2045424753 @default.
• W16282495 cites W2065051523 @default.
• W16282495 cites W2067995235 @default.
• W16282495 cites W2102777270 @default.
• W16282495 cites W2118895498 @default.
• W16282495 cites W2147711224 @default.
• W16282495 cites W2168361498 @default.
• W16282495 cites W217319772 @default.
• W16282495 cites W2174963971 @default.
• W16282495 cites W2187384654 @default.
• W16282495 cites W2336439670 @default.
• W16282495 cites W2526118183 @default.
• W16282495 cites W32919641 @default.
• W16282495 cites W84134233 @default.
• W16282495 doi "https://doi.org/10.1016/b978-1-4832-8366-1.50020-0" @default.
• W16282495 hasPublicationYear "1980" @default.
• W16282495 type Work @default.
• W16282495 sameAs 16282495 @default.
• W16282495 citedByCount "1" @default.
• W16282495 crossrefType "book-chapter" @default.
• W16282495 hasAuthorship W16282495A5032614869 @default.
• W16282495 hasAuthorship W16282495A5083778726 @default.
• W16282495 hasConcept C121332964 @default.
• W16282495 hasConcept C122523270 @default.
• W16282495 hasConcept C127313418 @default.
• W16282495 hasConcept C12980444 @default.
• W16282495 hasConcept C13280743 @default.
• W16282495 hasConcept C134097258 @default.
• W16282495 hasConcept C143351421 @default.
• W16282495 hasConcept C176341353 @default.
• W16282495 hasConcept C180205008 @default.
• W16282495 hasConcept C2779547961 @default.
• W16282495 hasConcept C43179477 @default.
• W16282495 hasConcept C43734619 @default.
• W16282495 hasConcept C44886760 @default.
• W16282495 hasConcept C49204034 @default.
• W16282495 hasConcept C62520636 @default.
• W16282495 hasConcept C73421765 @default.
• W16282495 hasConcept C8058405 @default.
• W16282495 hasConcept C91586092 @default.
• W16282495 hasConceptScore W16282495C121332964 @default.
• W16282495 hasConceptScore W16282495C122523270 @default.
• W16282495 hasConceptScore W16282495C127313418 @default.
• W16282495 hasConceptScore W16282495C12980444 @default.
• W16282495 hasConceptScore W16282495C13280743 @default.
• W16282495 hasConceptScore W16282495C134097258 @default.
• W16282495 hasConceptScore W16282495C143351421 @default.
• W16282495 hasConceptScore W16282495C176341353 @default.
• W16282495 hasConceptScore W16282495C180205008 @default.
• W16282495 hasConceptScore W16282495C2779547961 @default.
• W16282495 hasConceptScore W16282495C43179477 @default.
• W16282495 hasConceptScore W16282495C43734619 @default.
• W16282495 hasConceptScore W16282495C44886760 @default.
• W16282495 hasConceptScore W16282495C49204034 @default.
• W16282495 hasConceptScore W16282495C62520636 @default.
• W16282495 hasConceptScore W16282495C73421765 @default.
• W16282495 hasConceptScore W16282495C8058405 @default.
• W16282495 hasConceptScore W16282495C91586092 @default.
• W16282495 hasLocation W162824951 @default.
• W16282495 hasOpenAccess W16282495 @default.
• W16282495 hasPrimaryLocation W162824951 @default.
• W16282495 hasRelatedWork W13898892 @default.
• W16282495 hasRelatedWork W1488878721 @default.
• W16282495 hasRelatedWork W1976714553 @default.
• W16282495 hasRelatedWork W1997941296 @default.
• W16282495 hasRelatedWork W2018315430 @default.
• W16282495 hasRelatedWork W2024165666 @default.
• W16282495 hasRelatedWork W2026812752 @default.
• W16282495 hasRelatedWork W2034715771 @default.
• W16282495 hasRelatedWork W2048475581 @default.
• W16282495 hasRelatedWork W2052357112 @default.
• W16282495 hasRelatedWork W2064243816 @default.
• W16282495 hasRelatedWork W2136068826 @default.
• W16282495 hasRelatedWork W2168361498 @default.

• next