Ekman transport
= Ekman transport
{c}
{title2=$\mathbf M_E$}
{wiki}
<Ekman transport> is the depth-integrated <ageostrophic flow> in a frictional rotating <boundary layer>. Beneath a surface <stress> $\boldsymbol\tau$,
$$
\mathbf M_E=\frac{\boldsymbol\tau\times\widehat{\mathbf z}}{\rho f}
$$
with the stated orientation convention.