From: The vertical structure of annual wave energy flux in the tropical Indian Ocean
f = f0 + βy | Coriolis parameter |
\( N=\sqrt{-\left(g/{\rho}_0\right)\left(d\overline{\rho}/ dz\right)} \) | Buoyancy frequency |
x, y, z, t | Cartesian coordinates |
〈〈a, b, c〉〉 | Vector with x, y and z-axis components a, b, and c |
U ≡ 〈〈u, v, w〉〉 | Velocity vector |
∇ ≡ 〈〈∂x, ∂y, ∂z〉〉 | Gradient operator |
Φ | Geopotential |
q | Potential vorticity q ≡ vx − uy + [(f/N2)Φz]z |
φ | Solution of (6a) |
φapp | Solution of (7a) |
\( \left(\overline{u^2+{v}^2+{\Phi}_z^2/{N}^2}\right)/2 \) | Wave energy density |
μ = kx + mz − ωt | Wave phase |
k | Zonal wavenumber |
m | Vertical wavenumber |
ω | Wave frequency |
\( \overline{A} \) | Phase average of A |