The numerics of hydrostatic structured-grid coastal ocean models: State of the art and future perspectives

被引:69
作者
Klingbeil, Knut [1 ,2 ]
Lemarie, Florian [3 ]
Debreu, Laurent [3 ]
Burchard, Hans [2 ]
机构
[1] Univ Hamburg, Dept Math, Bundesstr 55, D-20146 Hamburg, Germany
[2] Leibniz Inst Baltic Sea Res Warnemunde, Seestr 15, D-18119 Rostock, Germany
[3] Univ Grenoble Alpes, CNRS, LJK, INRIA, F-38000 Grenoble, France
关键词
Coastal ocean models; Hydrostatic models; Adaptive coordinates; Mode-splitting; Drying & flooding; Two-way nesting; OPEN BOUNDARY-CONDITIONS; PRESSURE-GRADIENT FORCE; SEA-LEVEL RISE; MONOTONICITY-PRESERVING SCHEMES; ROTATED DIFFUSION OPERATORS; ESTUARINE TURBIDITY MAXIMA; GENERAL-CIRCULATION MODEL; TURBULENCE CLOSURE MODELS; INERTIA-GRAVITY WAVES; SIGMA-CO-ORDINATE;
D O I
10.1016/j.ocemod.2018.01.007
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The state of the art of the numerics of hydrostatic structured-grid coastal ocean models is reviewed here. First, some fundamental differences in the hydrodynamics of the coastal ocean, such as the large surface elevation variation compared to the mean water depth, are contrasted against large scale ocean dynamics. Then the hydrodynamic equations as they are used in coastal ocean models as well as in large scale ocean models are presented, including parameterisations for turbulent transports. As steps towards discretisation, coordinate transformations and spatial discretisations based on a finite-volume approach are discussed with focus on the specific requirements for coastal ocean models. As in large scale ocean models, splitting of internal and external modes is essential also for coastal ocean models, but specific care is needed when drying & flooding of intertidal flats is included. As one obvious characteristic of coastal ocean models, open boundaries occur and need to be treated in a way that correct model forcing from outside is transmitted to the model domain without reflecting waves from the inside. Here, also new developments in two-way nesting are presented. Single processes such as internal inertia-gravity waves, advection and turbulence closure models are discussed with focus on the coastal scales. Some overview on existing hydrostatic structured-grid coastal ocean models is given, including their extensions towards non-hydrostatic models. Finally, an outlook on future perspectives is made.
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页码:80 / 105
页数:26
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