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We empirically found (see Section 6.5.2 below) that the quality of the above
approximation can be improved by adding a correction term of
r 3 / (1
r 2 )
to it. Thus, we finally get
r 3
rd
κ =
.
(6.17)
1
r 2
Recently Tanabe et al. (50) used some inequalities regarding the Bessel func-
tion ratio A d ( κ ) (3) to bound the solution to A d ( κ )= r as
r ( d
rd
2)
≤ κ ≤
r 2 .
1
r 2
1
Our solution (6.17) lies within these bounds, thus leading to a better theoret-
ical justification in retrospect.
The approximation in (6.17) could perhaps be made even more accurate
by adding other correction terms that are functions of r and d . However, we
remark that if one wants a more accurate approximation, it is easier to use
(6.17) as a starting point and then perform Newton-Raphson iterations for
solving A d (
r = 0, since it is easy to evaluate A d ( κ )=1
A d ( κ ) 2
κ )
d− 1
κ A d ( κ ). However, for high-dimensional data, accurately computing A d ( κ )
can be quite slow compared to eciently approximating
κ using (6.17), and
a very high accuracy for κ is not that critical. For other approximations of κ
and some related issues, the reader is referred to (21; 5).
We now show some numerical results to assess the quality of our approxima-
tion in comparison to (6.14) and (6.15). First note that a particular value of r
may correspond to many different combinations of κ and d values. Then, one
needs to evaluate the accuracy of the approximations over the parts of the d - κ
plane that are expected to be encountered in the target application domains.
Section 6.5.2 below provides such an assessment by comparing performances
over different slices of the d - κ plane and over a range of r values. Below we
simply compare the accuracies at a set of points on this plane via Table 6.1
which shows the actual numerical values of κ that the three approximations
(6.14), (6.15), and (6.17) yielded at these points. The r values shown in the
table were computed using (6.5).
TABLE 6.1:
κ for a sampling of κ and d
Approximations
values.
( d, r, κ )
κ in (6.14)
κ in (6.15)
κ in (6.17)
(10 , 0 . 633668 , 10)
12 . 3
9 . 4
10 . 2
(100 , 0 . 46945 , 60)
93 . 3
59 . 4
60 . 1
(500 , 0 . 46859 , 300)
469 . 5
296 . 8
300 . 1
(1000 , 0 . 554386 , 800)
1120 . 9
776 . 8
800 . 1
 
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