Matches in SemOpenAlex for { <https://semopenalex.org/work/W2072853764> ?p ?o ?g. }
- W2072853764 endingPage "827" @default.
- W2072853764 startingPage "795" @default.
- W2072853764 abstract "Recent contributions to second-order turbulence modelling are reviewed with an emphasis on models of the coastal ocean. Classical and recent turbulence models are reformulated using a unifying notation, making differences in model structure and model parameters more transparent. The essential characteristics of a number of models are compared. It is further demonstrated that the mathematical stability and realisability of the models is crucial for practical applications. The parameter constraints to insure stable computations are discussed. Model performance is evaluated for a number of idealised entrainment scenarios that are typical for shelf seas: entrainment in linearly stratified and two-layer fluids caused by (a) surface wind stress (b) bottom stress due to water motion driven by a barotropic pressure gradient (c) bottom stress due to water motion in a bottom jet. It is shown that the predicted entrainment velocities are in good agreement with available laboratory data, provided the models have been calibrated according to a theoretical constraint. In addition, model behaviour in free convection is re-analysed with the help of recent data from large eddy simulations (LES). It is shown that even the most simple models, which do not solve a differential equation for the turbulent kinetic energy (TKE), can approximately reproduce the entrainment depth, however, they fail completely in reproducing the correct budget of the TKE-balance. In contrast, second-order models solving transport equations for the TKE and a length scale determining variable are in reasonable agreement with the TKE-budgets from LES." @default.
- W2072853764 created "2016-06-24" @default.
- W2072853764 creator A5017611951 @default.
- W2072853764 creator A5090457938 @default.
- W2072853764 date "2005-05-01" @default.
- W2072853764 modified "2023-10-18" @default.
- W2072853764 title "Second-order turbulence closure models for geophysical boundary layers. A review of recent work" @default.
- W2072853764 cites W1609323367 @default.
- W2072853764 cites W1622870125 @default.
- W2072853764 cites W1963549306 @default.
- W2072853764 cites W1963732111 @default.
- W2072853764 cites W1964574891 @default.
- W2072853764 cites W1965823081 @default.
- W2072853764 cites W1977126679 @default.
- W2072853764 cites W1977314054 @default.
- W2072853764 cites W1977362444 @default.
- W2072853764 cites W1981121301 @default.
- W2072853764 cites W1982040901 @default.
- W2072853764 cites W1987140621 @default.
- W2072853764 cites W1991121489 @default.
- W2072853764 cites W1991142423 @default.
- W2072853764 cites W1991923541 @default.
- W2072853764 cites W1997238803 @default.
- W2072853764 cites W1997997020 @default.
- W2072853764 cites W2004186030 @default.
- W2072853764 cites W2007519486 @default.
- W2072853764 cites W2016216840 @default.
- W2072853764 cites W2016644205 @default.
- W2072853764 cites W2016831994 @default.
- W2072853764 cites W2019584264 @default.
- W2072853764 cites W2025253577 @default.
- W2072853764 cites W2026119697 @default.
- W2072853764 cites W2028149208 @default.
- W2072853764 cites W2031127053 @default.
- W2072853764 cites W2034198478 @default.
- W2072853764 cites W2038742869 @default.
- W2072853764 cites W2042673419 @default.
- W2072853764 cites W2044886439 @default.
- W2072853764 cites W2050089774 @default.
- W2072853764 cites W2053074277 @default.
- W2072853764 cites W2055573138 @default.
- W2072853764 cites W2060917053 @default.
- W2072853764 cites W2061219759 @default.
- W2072853764 cites W2062474936 @default.
- W2072853764 cites W2068076894 @default.
- W2072853764 cites W2071669046 @default.
- W2072853764 cites W2074473161 @default.
- W2072853764 cites W2077391889 @default.
- W2072853764 cites W2078804147 @default.
- W2072853764 cites W2081868909 @default.
- W2072853764 cites W2083045724 @default.
- W2072853764 cites W2083778668 @default.
- W2072853764 cites W2089810834 @default.
- W2072853764 cites W2089970046 @default.
- W2072853764 cites W2090559027 @default.
- W2072853764 cites W2095018528 @default.
- W2072853764 cites W2101918617 @default.
- W2072853764 cites W2103340042 @default.
- W2072853764 cites W2108085782 @default.
- W2072853764 cites W2113264898 @default.
- W2072853764 cites W2114141131 @default.
- W2072853764 cites W2118187911 @default.
- W2072853764 cites W2119603362 @default.
- W2072853764 cites W2119643349 @default.
- W2072853764 cites W2127196447 @default.
- W2072853764 cites W2127447998 @default.
- W2072853764 cites W2129507136 @default.
- W2072853764 cites W2129602274 @default.
- W2072853764 cites W2136908941 @default.
- W2072853764 cites W2151078270 @default.
- W2072853764 cites W2163970160 @default.
- W2072853764 cites W2168346748 @default.
- W2072853764 cites W2169899461 @default.
- W2072853764 cites W2171454630 @default.
- W2072853764 cites W2173808101 @default.
- W2072853764 cites W2175356480 @default.
- W2072853764 cites W2176583222 @default.
- W2072853764 cites W2176770911 @default.
- W2072853764 cites W2176806292 @default.
- W2072853764 cites W2178641373 @default.
- W2072853764 cites W2179708439 @default.
- W2072853764 cites W4229999962 @default.
- W2072853764 cites W4232268884 @default.
- W2072853764 doi "https://doi.org/10.1016/j.csr.2004.08.004" @default.
- W2072853764 hasPublicationYear "2005" @default.
- W2072853764 type Work @default.
- W2072853764 sameAs 2072853764 @default.
- W2072853764 citedByCount "322" @default.
- W2072853764 countsByYear W20728537642012 @default.
- W2072853764 countsByYear W20728537642013 @default.
- W2072853764 countsByYear W20728537642014 @default.
- W2072853764 countsByYear W20728537642015 @default.
- W2072853764 countsByYear W20728537642016 @default.
- W2072853764 countsByYear W20728537642017 @default.
- W2072853764 countsByYear W20728537642018 @default.
- W2072853764 countsByYear W20728537642019 @default.
- W2072853764 countsByYear W20728537642020 @default.
- W2072853764 countsByYear W20728537642021 @default.