DJL equations: Difference between revisions
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== Non-Boussinesq constant background current <math>U_0</math> == | == Non-Boussinesq constant background current <math>U_0</math> == | ||
<math>\nabla^2\eta + \frac{N^2(z-\eta)}{U_0^2}\eta +\frac{N^2(z-\eta)}{2g}\left[\eta_x^2 +\eta_z(\eta_z-2)\right]</math> | <math>\nabla^2\eta + \frac{N^2(z-\eta)}{U_0^2}\eta +\frac{N^2(z-\eta)}{2g}\left[\eta_x^2 +\eta_z(\eta_z-2)\right] =0</math> | ||
where <math> N^2(z) = \frac{-g\bar{\rho}'(z)}{\bar{\rho}(z)}</math> | where <math> N^2(z) = \frac{-g\bar{\rho}'(z)}{\bar{\rho}(z)}</math> |
Revision as of 10:40, 7 July 2011
The Dubreil-Jacotin-Long (DJL) equation is derived from the steady Euler equations. The result is a single equation for the isopycnal displacement . Here are a few cases:
Boussinesq with constant background current
where . is the far upstream density profile, is a constant reference density ,and is the acceleration due to gravity.
Boussinesq with non-constant background current
Non-Boussinesq constant background current
where