Matches in SemOpenAlex for { <https://semopenalex.org/work/W2014108596> ?p ?o ?g. }
Showing items 1 to 56 of
56
with 100 items per page.
- W2014108596 endingPage "1432" @default.
- W2014108596 startingPage "1414" @default.
- W2014108596 abstract "Abstract A simple two-level model is designed to simulate the “thermocline equations,” applicable for large-scale steady oceanic flow. The model serves two functions. First, it replaces problems with the interpretation of slablike dynamics (e.g., Luyten et al., 1983) by using continuously horizontally varying buoyancy, but at the cost of reducing the vertical resolution drastically. The equations used are geostrophy (plus a small linear drag to close a Stommel-like western boundary layer), mass conservation, and buoyancy conservation with a small but necessary horizontal diffusion. (Inclusion of vertical diffusion has little effect). The ocean is driven by an Ekman layer, whose functions are to provide a given surface input of mass (through Ekman pumping) and buoyancy (through a specified buoyancy in the Ekman layer), i.e., to maintain the same boundary conditions as in classical thermocline studies. Sidewall conditions are not well understood and are almost certainly over-specified in this formulation. S..." @default.
- W2014108596 created "2016-06-24" @default.
- W2014108596 creator A5062102315 @default.
- W2014108596 date "1985-11-01" @default.
- W2014108596 modified "2023-09-26" @default.
- W2014108596 title "A Two-Level Wind and Buoyancy Driven Thermocline Model" @default.
- W2014108596 doi "https://doi.org/10.1175/1520-0485(1985)015<1414:atlwab>2.0.co;2" @default.
- W2014108596 hasPublicationYear "1985" @default.
- W2014108596 type Work @default.
- W2014108596 sameAs 2014108596 @default.
- W2014108596 citedByCount "33" @default.
- W2014108596 countsByYear W20141085962013 @default.
- W2014108596 crossrefType "journal-article" @default.
- W2014108596 hasAuthorship W2014108596A5062102315 @default.
- W2014108596 hasBestOaLocation W20141085961 @default.
- W2014108596 hasConcept C105824904 @default.
- W2014108596 hasConcept C111368507 @default.
- W2014108596 hasConcept C121332964 @default.
- W2014108596 hasConcept C127313418 @default.
- W2014108596 hasConcept C153294291 @default.
- W2014108596 hasConcept C39432304 @default.
- W2014108596 hasConcept C49204034 @default.
- W2014108596 hasConcept C538625479 @default.
- W2014108596 hasConcept C57879066 @default.
- W2014108596 hasConcept C91586092 @default.
- W2014108596 hasConceptScore W2014108596C105824904 @default.
- W2014108596 hasConceptScore W2014108596C111368507 @default.
- W2014108596 hasConceptScore W2014108596C121332964 @default.
- W2014108596 hasConceptScore W2014108596C127313418 @default.
- W2014108596 hasConceptScore W2014108596C153294291 @default.
- W2014108596 hasConceptScore W2014108596C39432304 @default.
- W2014108596 hasConceptScore W2014108596C49204034 @default.
- W2014108596 hasConceptScore W2014108596C538625479 @default.
- W2014108596 hasConceptScore W2014108596C57879066 @default.
- W2014108596 hasConceptScore W2014108596C91586092 @default.
- W2014108596 hasIssue "11" @default.
- W2014108596 hasLocation W20141085961 @default.
- W2014108596 hasOpenAccess W2014108596 @default.
- W2014108596 hasPrimaryLocation W20141085961 @default.
- W2014108596 hasRelatedWork W1703201332 @default.
- W2014108596 hasRelatedWork W1965332254 @default.
- W2014108596 hasRelatedWork W1968421303 @default.
- W2014108596 hasRelatedWork W2006377345 @default.
- W2014108596 hasRelatedWork W2014108596 @default.
- W2014108596 hasRelatedWork W2025435012 @default.
- W2014108596 hasRelatedWork W2034739610 @default.
- W2014108596 hasRelatedWork W2090440128 @default.
- W2014108596 hasRelatedWork W2172550942 @default.
- W2014108596 hasRelatedWork W4214921412 @default.
- W2014108596 hasVolume "15" @default.
- W2014108596 isParatext "false" @default.
- W2014108596 isRetracted "false" @default.
- W2014108596 magId "2014108596" @default.
- W2014108596 workType "article" @default.