1Ghil, M., Simonnet, E. (2020). Geophysical Fluid Dynamics, Nonautonomous Dynamical Systems, and the Climate Sciences.
2Nicole Sharp - August 21, 2024. Trapped in a Taylor Column.
3\(\frac{\partial u}{\partial z}
= \frac{\partial v}{\partial z}
= \frac{\partial u}{\partial x} + \frac{\partial v}{\partial y}
= 0 \Rightarrow \frac{\partial u}{\partial x}
+ \frac{\partial v}{\partial y}
+ \frac{\partial w}{\partial z}
= 0 \Rightarrow \frac{\partial w}{\partial z} = 0
\Rightarrow (2\boldsymbol{\Omega} \cdot \nabla)\mathbf{u} = 0\)
This constraint is called the Taylor-Proudman theorem. In this case all three components of the relative velocity are independent of the direction parallel to the rotation axis.
if \(w\) is zero at some level, for example at a rigid, horizontal surface, it remains zero for all \(z\). The motion is then completely two dimensional and can be pictured as moving in columns, each column oriented parallel to the rotation axis and moving so as to maintain this orientation. The columns themselves are most often referred to as Taylor columns.