Vector volume data contains more information than scalar data because each coordinate point in the data set has three values associated with it. These values define a vector that represents both a magnitude and a direction. The velocity of fluid flow is an example of vector data.
A number of techniques are useful for visualizing vector data:
Stream lines trace the path that a massless particle immersed in the vector field would follow.
Stream particles are markers that trace stream lines and are useful for creating stream line animations.
Stream ribbons are similar to stream lines, except that the width of the ribbons enables them to indicate twist. Stream ribbons are useful to indicate curl angular velocity.
Stream tubes are similar to stream lines, but you can also control the width of the tube. Stream tubes are useful for displaying the divergence of a vector field.
Cone plots represent the magnitude and direction of the data at each point by displaying a conical arrowhead or an arrow.
It is typically the case that these functions best elucidate the data when used in conjunction with other visualization techniques, such as contours, slice planes, and isosurfaces. The examples in this section illustrate some of these techniques.
Visualization techniques such as contour slices, slice planes,
and isosurfaces require scalar volume data. You can use these techniques
with vector data by taking the magnitude of the vectors. For example,
wind data set returns three coordinate arrays
and three vector component arrays,
In this case, the magnitude of the velocity vectors equals the wind
speed at each corresponding coordinate point in the volume.
wind_speed = sqrt(u.^2 + v.^2 + w.^2);
wind_speed contains scalar values
for the volume data. The usefulness of the information produced by
this approach, however, depends on what physical phenomenon is represented
by the magnitude of your vector data.
Stream plots (stream lines, ribbons, tubes, and cones or arrows)
illustrate the flow of a 3-D vector field. The MATLAB® stream-plotting
stream3) all require you to specify the
point at which you want to begin each stream trace.
Generally, knowledge of your data's characteristics helps you select the starting points. Information such as the primary direction of flow and the range of the data coordinates helps you decide where to evaluate the data.
is useful for exploring your data. For example, these statements draw
a slice through the vector field at a z value midway
in the range.
load wind zmax = max(z(:)); zmin = min(z(:)); streamslice(x,y,z,u,v,w,,,(zmax-zmin)/2)
This stream slice plot indicates that the flow is in the positive x-direction and also enables you to select starting points in both x and y. You could create similar plots that slice the volume in the x-z plane or the y-z plane to gain further insight into your data's range and orientation.
To specify the starting point for one stream line, you need
the x-, y-, and z-coordinates
of the point. The
provides a convenient way to create arrays of starting points. For
example, you could select the following starting points from the wind
data displayed in the previous stream slice.
[sx,sy,sz] = meshgrid(80,20:10:50,0:5:15);
This statement defines the starting points as all lying on x
= 80, y ranging from 20 to 50, and z ranging from 0 to 15. You can
plot3 to display the locations.
plot3(sx(:),sy(:),sz(:),'*r'); axis(volumebounds(x,y,z,u,v,w)) grid on set(gca,'BoxStyle','full','Box','on') daspect([2 2 1])
You do not need to use 3-D arrays, such as those returned by
but the size of each array must be the same, and
a convenient way to generate arrays when you do not have an equal
number of unique values in each coordinate. You can also define starting-point
arrays as column vectors. For example,
[sx,sy,sz] = meshgrid(80,20:10:50,0:5:15); whos
Name Size Bytes Class Attributes sx 4x1x4 128 double sy 4x1x4 128 double sz 4x1x4 128 double
In addition, you could use 16-by-1 column vectors with the corresponding
elements of the three arrays composing the coordinates of each starting
point. (This is the equivalent of indexing the values returned by
For example, adding the stream lines to the starting points produces:
provides a simple way to access subregions of a volume data set.
you to select regions of interest based on limits rather than using
the colon operator to index
into the 3-D arrays that define volumes. Consider the following two
approaches to creating the data for a subvolume — indexing
with the colon operator and using
When you index the arrays, you work with values that specify the elements in each dimension of the array.
load wind xsub = x(1:10,20:30,1:7); ysub = y(1:10,20:30,1:7); zsub = z(1:10,20:30,1:7); usub = u(1:10,20:30,1:7); vsub = v(1:10,20:30,1:7); wsub = w(1:10,20:30,1:7);
subvolume enables you to use coordinate values
that you can read from the axes. For example:
lims = [100.64 116.67 17.25 28.75 -0.02 6.86]; [xsub,ysub,zsub,usub,vsub,wsub] = subvolume(x,y,z,u,v,w,lims);
You can then use the subvolume data as inputs to any function requiring vector volume data.