2001
DOI: 10.1175/1520-0485(2001)031<0094:atdbmo>2.0.co;2
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A Three-Dimensional Baroclinic Model of the Irish Sea: Formation of the Thermal Fronts and Associated Circulation

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Cited by 67 publications
(117 citation statements)
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“…The first reproduction of the western Irish Sea gyre was obtained by the application of a threedimensional diagnostic model, giving good agreement with previous observations, Hill et al (1996), Hill et al (1997). Horsburgh (1999), Xing and Davies (2001) and Horsburgh and Hill (2003) applied a three-dimensional density-resolving model and succeeded to predict the gyre in a prognostic manner. Good agreement was achieved, and the accuracy of temperature field prediction depended on the advection scheme implemented and the choice of turbulent model parameters.…”
Section: Introductionsupporting
confidence: 78%
“…The first reproduction of the western Irish Sea gyre was obtained by the application of a threedimensional diagnostic model, giving good agreement with previous observations, Hill et al (1996), Hill et al (1997). Horsburgh (1999), Xing and Davies (2001) and Horsburgh and Hill (2003) applied a three-dimensional density-resolving model and succeeded to predict the gyre in a prognostic manner. Good agreement was achieved, and the accuracy of temperature field prediction depended on the advection scheme implemented and the choice of turbulent model parameters.…”
Section: Introductionsupporting
confidence: 78%
“…The vertical velocity ω, which appears in the threedimensional advection terms, is obtained diagnostically from the continuity equation (Xing and Davies 2001b), with the pressure P at any depth σ given by…”
Section: The Three-dimensional Non-linear Numerical Modelmentioning
confidence: 99%
“…The terms S U , S V , S T represent the full three-dimensional momentum advection terms, with D U , D V , D T the horizontal diffusion terms. Details of the mathematical formulation of these terms are given in Xing and Davies (2001b). Horizontal viscosity (A m ) and diffusivity (A h ) were given by A m =100 m 2 s −1 and A h =100 m 2 s −1 .…”
Section: The Three-dimensional Non-linear Numerical Modelmentioning
confidence: 99%
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“…As they are discussed in detail in Xing and Davies (2001b) they will not be repeated here, except to give a general overview of their basic form.…”
Section: The Hydrodynamic Equations Topography Of the Region And Chmentioning
confidence: 99%