FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2119506743> ?p ?o ?g. }

• W2119506743 endingPage "3158" @default.
• W2119506743 startingPage "3139" @default.
• W2119506743 abstract "The mean and turbulent structures in a breaking mountain wave are considered through an ensemble of high-resolution (essentially large-eddy simulation) wave-breaking calculations. Of particular interest are the turbulent heat and momentum fluxes in the breaking wave and their roles in shaping the wave-scale and larger-scale flows. The evolution of the breaking wave in the ensemble mean is found to be broadly consistent with prior low-resolution calculations. A turbulent kinetic energy budget for the wave shows that the turbulence production is almost entirely due to the mean shear. Most of the production is at the top of the leeside shooting flow, where the mean-flow Richardson number is persistently less than 0.25. The turbulent dissipation of mean-flow wave energy is shown to result mainly from the turbulent momentum fluxes—specifically, from the tendency of these fluxes to act counter to the mean-flow disturbance wind. Of particular importance is the eddy deceleration of the leeside shooting flow. The resulting momentum dissipation leads to a mean-flow Bernoulli loss, a cross-stream mean-flow PV flux, and a permanent upward mean-flow vorticity transfer. The dependence of the turbulent fluxes on grid spacing is considered by computing a series of ensembles with grid spacings ranging from L/56 to L/3.7 (where L is the mountain half-width). At the highest resolution, the eddy fluxes are mostly resolved, but with increasing grid spacing, the resolved-scale fluxes decline and the parameterized fluxes become larger. It is shown that for the chosen parameter values, the parameterized fluxes overestimate the mean-flow PV flux: at L/3.7 the PV flux is nearly twice that computed at L/56." @default.
• W2119506743 created "2016-06-24" @default.
• W2119506743 creator A5002010245 @default.
• W2119506743 creator A5046811221 @default.
• W2119506743 date "2008-10-01" @default.
• W2119506743 modified "2023-10-10" @default.
• W2119506743 title "Wave–Turbulence Interactions in a Breaking Mountain Wave" @default.
• W2119506743 cites W1967003258 @default.
• W2119506743 cites W1967297839 @default.
• W2119506743 cites W1967329175 @default.
• W2119506743 cites W1987735184 @default.
• W2119506743 cites W1988560105 @default.
• W2119506743 cites W1989788229 @default.
• W2119506743 cites W1992082987 @default.
• W2119506743 cites W1993962576 @default.
• W2119506743 cites W2000757858 @default.
• W2119506743 cites W2001593012 @default.
• W2119506743 cites W2032290081 @default.
• W2119506743 cites W2044751363 @default.
• W2119506743 cites W2047343867 @default.
• W2119506743 cites W2051368762 @default.
• W2119506743 cites W2055484525 @default.
• W2119506743 cites W2073609093 @default.
• W2119506743 cites W2076984229 @default.
• W2119506743 cites W2088521789 @default.
• W2119506743 cites W2094214703 @default.
• W2119506743 cites W2100877846 @default.
• W2119506743 cites W2104102786 @default.
• W2119506743 cites W2105841507 @default.
• W2119506743 cites W2108889917 @default.
• W2119506743 cites W2114152926 @default.
• W2119506743 cites W2126882530 @default.
• W2119506743 cites W2131187765 @default.
• W2119506743 cites W2134450492 @default.
• W2119506743 cites W2144131962 @default.
• W2119506743 cites W2144647782 @default.
• W2119506743 cites W2155657556 @default.
• W2119506743 cites W2160104288 @default.
• W2119506743 cites W2167801319 @default.
• W2119506743 cites W2169993534 @default.
• W2119506743 cites W2172471442 @default.
• W2119506743 cites W2174296419 @default.
• W2119506743 cites W2174400063 @default.
• W2119506743 cites W2180102330 @default.
• W2119506743 doi "https://doi.org/10.1175/2008jas2517.1" @default.
• W2119506743 hasPublicationYear "2008" @default.
• W2119506743 type Work @default.
• W2119506743 sameAs 2119506743 @default.
• W2119506743 citedByCount "21" @default.
• W2119506743 countsByYear W21195067432012 @default.
• W2119506743 countsByYear W21195067432013 @default.
• W2119506743 countsByYear W21195067432014 @default.
• W2119506743 countsByYear W21195067432015 @default.
• W2119506743 countsByYear W21195067432016 @default.
• W2119506743 countsByYear W21195067432017 @default.
• W2119506743 countsByYear W21195067432018 @default.
• W2119506743 countsByYear W21195067432020 @default.
• W2119506743 countsByYear W21195067432021 @default.
• W2119506743 countsByYear W21195067432022 @default.
• W2119506743 crossrefType "journal-article" @default.
• W2119506743 hasAuthorship W2119506743A5002010245 @default.
• W2119506743 hasAuthorship W2119506743A5046811221 @default.
• W2119506743 hasBestOaLocation W21195067431 @default.
• W2119506743 hasConcept C10138342 @default.
• W2119506743 hasConcept C120665830 @default.
• W2119506743 hasConcept C121332964 @default.
• W2119506743 hasConcept C135402231 @default.
• W2119506743 hasConcept C140820882 @default.
• W2119506743 hasConcept C153294291 @default.
• W2119506743 hasConcept C15476950 @default.
• W2119506743 hasConcept C157331469 @default.
• W2119506743 hasConcept C162324750 @default.
• W2119506743 hasConcept C169596890 @default.
• W2119506743 hasConcept C191486275 @default.
• W2119506743 hasConcept C196558001 @default.
• W2119506743 hasConcept C200114574 @default.
• W2119506743 hasConcept C205904022 @default.
• W2119506743 hasConcept C44886760 @default.
• W2119506743 hasConcept C57879066 @default.
• W2119506743 hasConcept C60718061 @default.
• W2119506743 hasConcept C76494280 @default.
• W2119506743 hasConcept C91586092 @default.
• W2119506743 hasConcept C97355855 @default.
• W2119506743 hasConceptScore W2119506743C10138342 @default.
• W2119506743 hasConceptScore W2119506743C120665830 @default.
• W2119506743 hasConceptScore W2119506743C121332964 @default.
• W2119506743 hasConceptScore W2119506743C135402231 @default.
• W2119506743 hasConceptScore W2119506743C140820882 @default.
• W2119506743 hasConceptScore W2119506743C153294291 @default.
• W2119506743 hasConceptScore W2119506743C15476950 @default.
• W2119506743 hasConceptScore W2119506743C157331469 @default.
• W2119506743 hasConceptScore W2119506743C162324750 @default.
• W2119506743 hasConceptScore W2119506743C169596890 @default.
• W2119506743 hasConceptScore W2119506743C191486275 @default.
• W2119506743 hasConceptScore W2119506743C196558001 @default.
• W2119506743 hasConceptScore W2119506743C200114574 @default.
• W2119506743 hasConceptScore W2119506743C205904022 @default.
• W2119506743 hasConceptScore W2119506743C44886760 @default.

• next