Matches in SemOpenAlex for { <https://semopenalex.org/work/W1966381311> ?p ?o ?g. }
Showing items 1 to 89 of
89
with 100 items per page.
- W1966381311 endingPage "2936" @default.
- W1966381311 startingPage "2909" @default.
- W1966381311 abstract "A strong, isolated October storm generated 0.35–0.7 m s−1 inertia] frequency currents in the 40-m deep mixed layer of a 300 km×300 km region of the northeast Pacific Ocean. The authors describe the evolution of these currents and the background flow in which they evolve for nearly a month following the storm. Instruments included CTD profilers, 36 surface drifters, an array of 7 moorings, and air-deployed velocity profilers. The authors then test whether the theory of linear internal waves propagating in a homogeneous ocean can explain the observed evolution of the inertial frequency currents. The subinertial frequency flow is weak, with typical currents of 5 cm s−1, and steady over the period of interest. The storm generates inertial frequency currents in and somewhat below the mixed layer with a horizontal scale much larger than the Rossby radius of deformation, reflecting the large-scale and rapid translation speed of the storm. This scale is too large for significant linear propagation of the inertial currents to occur. It steadily decreases owing to the latitudinal variation in f, that is, β, until after about 10 days it becomes sufficiently small for wave propagation to occur. Inertial energy then spreads downward from the mixed layer, decreasing the mixed layer inertial energy and increasing the inertial energy below the mixed layer. A strong maximum in inertial energy is formed at 100 m (the Beam). By 21 days after the storm. both mixed layer inertial energy and inertial frequency shear maximum just below the mixed layer have been reduced to background levels. The total depth-average inertial energy decreases by about 40% during this period. Linear internal wave theory can only partially explain the observed evolution of the inertial frequency currents. The decrease in horizontal wavelength is accurately predicted as due to the β effect. The decrease in depth-average inertial energy is explained by southward propagation of the lowest few modes. The superinertial frequency and clockwise rotation of phase with depth are qualitatively consistent with linear theory. However, linear theory underpredicts the initial rate at which inertial energy is lost from the mixed layer by 20%–50% and cannot explain the decrease of mixed layer energy and shear to background levels in 21 days." @default.
- W1966381311 created "2016-06-24" @default.
- W1966381311 creator A5011355409 @default.
- W1966381311 creator A5019732929 @default.
- W1966381311 creator A5022701276 @default.
- W1966381311 creator A5054131652 @default.
- W1966381311 creator A5063539271 @default.
- W1966381311 creator A5082130798 @default.
- W1966381311 date "1995-11-01" @default.
- W1966381311 modified "2023-10-14" @default.
- W1966381311 title "Upper-Ocean Inertial Currents Forced by a Strong Storm. Part I: Data and Comparisons with Linear Theory" @default.
- W1966381311 doi "https://doi.org/10.1175/1520-0485(1995)025<2909:uoicfb>2.0.co;2" @default.
- W1966381311 hasPublicationYear "1995" @default.
- W1966381311 type Work @default.
- W1966381311 sameAs 1966381311 @default.
- W1966381311 citedByCount "171" @default.
- W1966381311 countsByYear W19663813112012 @default.
- W1966381311 countsByYear W19663813112013 @default.
- W1966381311 countsByYear W19663813112014 @default.
- W1966381311 countsByYear W19663813112015 @default.
- W1966381311 countsByYear W19663813112016 @default.
- W1966381311 countsByYear W19663813112017 @default.
- W1966381311 countsByYear W19663813112018 @default.
- W1966381311 countsByYear W19663813112019 @default.
- W1966381311 countsByYear W19663813112020 @default.
- W1966381311 countsByYear W19663813112021 @default.
- W1966381311 countsByYear W19663813112022 @default.
- W1966381311 countsByYear W19663813112023 @default.
- W1966381311 crossrefType "journal-article" @default.
- W1966381311 hasAuthorship W1966381311A5011355409 @default.
- W1966381311 hasAuthorship W1966381311A5019732929 @default.
- W1966381311 hasAuthorship W1966381311A5022701276 @default.
- W1966381311 hasAuthorship W1966381311A5054131652 @default.
- W1966381311 hasAuthorship W1966381311A5063539271 @default.
- W1966381311 hasAuthorship W1966381311A5082130798 @default.
- W1966381311 hasBestOaLocation W19663813111 @default.
- W1966381311 hasConcept C105306849 @default.
- W1966381311 hasConcept C121332964 @default.
- W1966381311 hasConcept C122120755 @default.
- W1966381311 hasConcept C127313418 @default.
- W1966381311 hasConcept C143351421 @default.
- W1966381311 hasConcept C153294291 @default.
- W1966381311 hasConcept C173386949 @default.
- W1966381311 hasConcept C43179477 @default.
- W1966381311 hasConcept C43734619 @default.
- W1966381311 hasConcept C44886760 @default.
- W1966381311 hasConcept C49204034 @default.
- W1966381311 hasConcept C57879066 @default.
- W1966381311 hasConcept C62520636 @default.
- W1966381311 hasConcept C74650414 @default.
- W1966381311 hasConcept C8058405 @default.
- W1966381311 hasConcept C91586092 @default.
- W1966381311 hasConceptScore W1966381311C105306849 @default.
- W1966381311 hasConceptScore W1966381311C121332964 @default.
- W1966381311 hasConceptScore W1966381311C122120755 @default.
- W1966381311 hasConceptScore W1966381311C127313418 @default.
- W1966381311 hasConceptScore W1966381311C143351421 @default.
- W1966381311 hasConceptScore W1966381311C153294291 @default.
- W1966381311 hasConceptScore W1966381311C173386949 @default.
- W1966381311 hasConceptScore W1966381311C43179477 @default.
- W1966381311 hasConceptScore W1966381311C43734619 @default.
- W1966381311 hasConceptScore W1966381311C44886760 @default.
- W1966381311 hasConceptScore W1966381311C49204034 @default.
- W1966381311 hasConceptScore W1966381311C57879066 @default.
- W1966381311 hasConceptScore W1966381311C62520636 @default.
- W1966381311 hasConceptScore W1966381311C74650414 @default.
- W1966381311 hasConceptScore W1966381311C8058405 @default.
- W1966381311 hasConceptScore W1966381311C91586092 @default.
- W1966381311 hasIssue "11" @default.
- W1966381311 hasLocation W19663813111 @default.
- W1966381311 hasOpenAccess W1966381311 @default.
- W1966381311 hasPrimaryLocation W19663813111 @default.
- W1966381311 hasRelatedWork W1969349190 @default.
- W1966381311 hasRelatedWork W2043879623 @default.
- W1966381311 hasRelatedWork W2065921574 @default.
- W1966381311 hasRelatedWork W2156387064 @default.
- W1966381311 hasRelatedWork W2156692262 @default.
- W1966381311 hasRelatedWork W2363121939 @default.
- W1966381311 hasRelatedWork W2998655981 @default.
- W1966381311 hasRelatedWork W3125070615 @default.
- W1966381311 hasRelatedWork W3206954486 @default.
- W1966381311 hasRelatedWork W4240079397 @default.
- W1966381311 hasVolume "25" @default.
- W1966381311 isParatext "false" @default.
- W1966381311 isRetracted "false" @default.
- W1966381311 magId "1966381311" @default.
- W1966381311 workType "article" @default.