Several parameters can be animated to improve the visualization. An animated offset vector o (see Sect. 4.3 and Fig. 4.8) is used to move stream arrows along stream lines within the stream surface. Composing the tiles of the texture in a regular manner, just a few images of the animation sequence have to be rendered. A longer sequence can be produced by looping the cyclic sequence several times.
Other sequences are rendered by animating the construction of a
stream surface. The temporal evolution of a stream surface
starting from an initial set of colinear points is illustrated.
Taking the stream surface of the mixed-mode oscillations model to
be opaque clearly shows how some parts of the model representation
severely occlude other portions. With stream arrows this
unsatisfactory situation is improved. The animation of the
stream surface evolution gives a good impression of the dynamics
induced by the given dynamical system.
The removal of certain parts of the model can be animated as well.
A simulated process of successively removing more and more parts
of the stream surface is easier to interpret than still images
where parts of the model have been removed. Another animation
sequence we rendered shows such a process--a cut plane is
used to distinguish semi-transparent parts of the stream surface
above the plane from opaque areas below. During the animation the
plane is moved towards the center of the model, so that
successively most parts of the stream surface become visible.
Many other parameters are suitable to be animated. Moving
the viewpoint around the model does certainly help to understand
the system behavior. The initial curve of the constructed stream
surface may be moved to demonstrate stability features of the
dynamical system. This corresponds to successively displaying not
only one but various adjacent stream surfaces. The stream lines
used to enhance the edges of the stream surface could be animated
by moving their origins along the line of initial conditions.
This would improve the visualization of the flow within a stream
surface.