Integral nonlinearity

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In statistics, the Bingham distribution, named after Christopher Bingham, is an antipodally symmetric probability distribution on the n-sphere.[1]

It is widely used in paleomagnetic data analysis,[2] and has been reported as being of use in the field of computer vision.[3][4]

Its probability density function is given by

f(x;M,Z)dSn1=1F1(12;n2;Z)1exp(trZMTxxTM)dSn1

which may also be written

f(x;M,Z)dSn1=1F1(12;n2;Z)1exp(xTMZMTx)dSn1

where x is an axis, M is an orthogonal orientation matrix, Z is a diagonal concentration matrix, 1F1(;,) is a confluent hypergeometric function of matrix argument.

See also

References

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  1. Bingham, Ch. (1974) "An antipodally symmetric distribution on the sphere". Annals of Statistics, 2(6):1201–1225.
  2. Onstott, T.C. (1980) "Application of the Bingham distribution function in paleomagnetic studies". Journal of Geophysical Research, 85:1500–1510.
  3. Template:Cite web
  4. Template:Cite web