Zones are topologically equivalent families of iso-surface bounded objects; zone components contain topologically equivalent families of iso-surfaces
1) For each
satisfying
,
is contained in
and
each component M of
is contained in a single
component of
.
2) For any pair
,
and
are homeomorphic.
3) For all
,
if O is any component of
not containing
p, then B (O) and
are disjoint.
4) For any
such that
or
,
and
are disjoint.
Proof: A pointif and only if f(q) < f(r) < f(p) and
. For
,
consists of points r with
, and by monotonicity of
each such
, so that that
is contained in
. The connectivity of M insures that it is contained in a single component of
, establishing claim 1.
By the definitions of the criticality graph and the zones,contains no critical point with value between f(p) and f(q); this establishes claim 2.
Claim 3 follows from the connectivity ofand the fact that boundary manifolds are pairwise disjoint by axiom 1.
Claim 4 follows immediately from the proof of claim 1.
Observe that, by the continuity of f and the monotonicity of the level sets
as the threshold is decreased, one can show that
will have one component
for each boundary iso-surface of
,
for
.
The theorem suggests a powerful way to organize the data readings, and means that we can simplify the data in a zone without losing any essential topological information. The criticality graph, with the zones associated with each vertex, hierarchically organize the entire dataset (as opposed to [2]).
Since the zone
of criticality p represents a collection
of topologically identical level set components (objects),
we can thus trace an object's evolution, as the threshold is varied, using the criticality graph.
To summarize:
The following hold:
Each node in the graph represents a topologically distinct family of objects (over all thresholds). Each object is associated with a node in the graph.
Proof: The results follow immediately from theorems 2 and 3, and the definition of the criticality graph.![]()