Bernoulli equation over topography
= Bernoulli equation over topography
{c}
For steady potential flow over small hills, linearized Bernoulli pressure combines a hydrostatic term $-\rho g\eta$ with a dynamic term $-\rho U\phi_x$.
= Bernoulli equation over topography
{c}
For steady potential flow over small hills, linearized Bernoulli pressure combines a hydrostatic term $-\rho g\eta$ with a dynamic term $-\rho U\phi_x$.