The evolution of finite-time singular vectors growing on four-dimensional s
pace-time basic states is studied for cases of block development over the G
ulf of Alaska and over the North Atlantic, using a two-level tangent linear
model. The initial singular vectors depend quite sensitively on the choice
of norm with the streamfunction norm characterized by small-scale baroclin
ic disturbances, the kinetic energy norm giving intermediate-scale baroclin
ic disturbances, and the enstophy norm typified by large-scale disturbances
with large zonal Row contributions. In all cases, the final evolved singul
ar vectors consist of large-scale equivalent barotropic wave trains across
the respective blocking regions. There are close similarities between the e
volved singular vectors in each of the norms, particularly for the longer t
ime periods considered, and with corresponding evolved finite-time adjoint
modes and evolved maximum sensitivity perturbations. For the longer time pe
riods considered, each of these evolved perturbations also closely resemble
s some of the dominant finite-time normal mode disturbances, which are norm
independent. For periods between about two weeks and a month, the converge
nce of the evolved leading singular vector and leading finite-time normal m
ode toward the leading left Lyapunov vector has been examined.
The evolution of errors, represented by singular vectors, is also considere
d in the space of finite-time normal modes. In all cases the evolved error
dynamics contracts onto a low-dimensional subspace characterized by the dom
inant finite-time normal modes. The growth of norms based on streamfunction
. kinetic energy, or enstrophy is compared with the growth of a norm based
on the projection coefficients of the disturbance onto the dominant finite-
time normal modes.
The prospect of ensemble prediction schemes in which the control initial co
nditions are perturbed by superpositions of the dominant finite-time normal
modes is discussed.