Abstract-
The solution of linearized Navier-Stokes equations can be presented as an
expansion into normal modes of the discrete and continuous spectra.
In the case of an initial-value problem, the normal modes are associated with
the temporal stability theory, whereas in the case of a signaling problem,
they are associated with the spatial stability theory. Because the operator is
not self-adjoint, the normal modes are non-orthogonal. However, there is an
orthogonality (biorthogonality) condition for modes of the direct and adjoint
problems. The latter can serve as a filter to find out the amplitude and phase
of a mode in a perturbation field.
The biorthogonal eigenfunction system may serve as a tool for the analysis of
perturbations. Particularly, one can easily find the amplitude of an
instability mode generated by an oscillator in a boundary layer, or the
amplitude of a mode of the continuous spectrum generated by a hump on the wall.
Other applications are associated with the decomposition of a perturbation
field in a computational study. If some a priori information about the
perturbation is available, the method can be used for the decomposition of
experimental data when only partial measurements (for example, one velocity
component) are provided. The discussion is accompanied by illustrations for
low- and high-speed boundary layers.
The figure illustrates a theoretical flow-field downstream of a hump. The
solution is comprised of normal modes of the continuous spectrum. Vectors
represent perturbations of the spanwise and the normal, , velocity components,
whereas the contours represent perturbation of the streamwise velocity, u. One
can see the wake region behind the hump , and the high speed streaks, , at the
sides of the hump ( mm).

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