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Polar Sine


The polar sine is a function of a vertex angle of an n-dimensional parallelotope or simplex. If the content of the parallelotope is P and the lengths of the n edges of the parallelotope that meet at vertex V_0 are E_1, E_2, ..., E_n, then the value of the polar sine of that vertex is

 polsinV_0=P/(product_(k=1)^(n)E_k).

Changing the length of an edge of the parallelotope by a factor changes the content P 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 2^n 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 n-dimensional angle, the n rays of the angle intersect the sphere at n points that are the vertices of an (n-1)-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 n-dimensional spherical simplex S, if the edges between vertices V_i and V_j have length E_(ij), the value of its polar sine in space with Gaussian curvature K>0 is given by

 polsin^2S=|1 cosE_(01)sqrt(K) ... cosE_(0n)sqrt(K); cosE_(10)sqrt(K) 1 ... cosE_(1n)sqrt(K); | | ... |; cosE_(n0)sqrt(K) cosE_(n1)sqrt(K) ... 1|.

Let an n-dimensional spherical simplex lie on a sphere with center O, and construct its polar simplex. Then the n-dimensional angle at O formed by the rays from O 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 n-dimensional spherical simplex as the curvature K of the space approaches zero is n!SK^(n/2), where S is the content of the Euclidean simplex with the same edge lengths.


See also

Hyperbolic Polar Sine, Hypersine, Sine

This entry contributed by Robert A. Russell

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References

Eriksson, F. "The Law of Sines for Tetrahedra and n-Simplices." Geom. Dedicata 7, 71-80, 1978.

Referenced on Wolfram|Alpha

Polar Sine

Cite this as:

Russell, Robert A. "Polar Sine." From MathWorld--A Wolfram Web Resource, created by Eric W. Weisstein. https://mathworld.wolfram.com/PolarSine.html

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