The polar sine is a function of a vertex angle of an -dimensional parallelotope or simplex. If the content of the
parallelotope is
and the lengths of the
edges of the parallelotope that meet at vertex
are
,
, ...,
, then the value of the polar sine of that vertex is
Changing the length of an edge of the parallelotope by a factor changes the content by the same factor. Thus, a change in
edge length does not affect the value of the right-hand side, and the polar sine
function is dependent solely on the angles between the edges of the parallelotope,
not their lengths. Also the polar sines of all of the vertex angles of the parallelotope
are the same, since the right-hand side of the definition does not depend on the
vertex chosen. If we extend the facets at a vertex, all of the
vertex angles thus formed have the same polar sine, as they
are simply translations of the vertex angles of the parallelotope.
If a sphere is centered at the vertex of an -dimensional angle, the
rays of the angle intersect the sphere at
points that are the vertices of an
-dimensional spherical simplex that subtends the angle.
We define the polar sine of that spherical simplex to be the polar sine of the angle
it subtends. For an
-dimensional
spherical simplex
,
if the edges between vertices
and
have length
, the value of its polar sine in space with Gaussian
curvature
is given by
Let an -dimensional
spherical simplex lie on a sphere with center
, and construct its polar simplex. Then the
-dimensional angle at
formed by the rays from
through the vertices of the polar simplex has a sine value
that is equal to the value of the polar sine of the original simplex.
The limit of the polar sine of an -dimensional spherical simplex as the curvature
of the space approaches zero is
, where
is the content of the Euclidean simplex with the same edge
lengths.