Non-Linear Dynamics and Statistical Theories for Basic Geophysical Flows

The purpose of this Appendix is to elaborate on the invariant dynamics on the first two energy shells. This is a special case of the exact dynamics of the ground state modes and the nth energy shell discussed in Subsection 16.2.1 with n = 2. For this purpose let us recall the following tables:
Eigenfunctions corresponding to ? ? 1= ?2( n=1)
Eigenfunctions corresponding to ? ? 2= ?6( n=2)
It is easy to see, utilizing (16.6)
This implies, since x 2 = 0.5( x 2 ? y 2) + 0.5(1 ? z 2) , that
This further implies, thanks to the rotation symmetry of the sphere and the eigenfunctions (which are homogeneous polynomials of degree 1 and 2),
Thus for
we have
We observe
Hence the dynamics of the coefficients are given by, for the simple case of no topography ( h = 0), no damping (
= 0) and no external forcing (
= 0)
This system of linear equations can be written in a compact form
where the matrix A is given by
In general the above matrix A is periodic in t with period ?/ ? (since a 1 1, b 11 are periodic in t with period ?/ ?) and Floquet theory is needed to solve such system.
Special Case 1: a 11 = a