Pages that link to "Item:Q3211070"
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The following pages link to A solution for the vertical variation of stress, rather than velocity, in a three-dimensional circulation model (Q3211070):
Displaying 5 items.
- A new method of describing bottom stress in two-dimensional hydrodynamical models of shallow homogeneous seas, estuaries, and lakes (Q1112659) (← links)
- A consistent formulation of the anisotropic stress tensor for use in models of the large-scale ocean circulation (Q1803293) (← links)
- On obtaining the steady-state solutions of the linearized three- dimensional hydrodynamic equations (Q1903229) (← links)
- Implicit finite volume simulation of 2D shallow water flows in flexible meshes (Q2310116) (← links)
- Analytic reconstruction of a two-dimensional velocity field from an observed diffusive scalar (Q5378193) (← links)