relate the arc length of an arc of the lemniscate to the distance of one endpoint from the origin. The determination of the
arc length of arcs of the lemniscate leads to
elliptic integrals, as was discovered in the eighteenth century. Around 1800, the
elliptic functions inverting those integrals were studied by
C. F. Gauss (largely unpublished at the time, but allusions in the notes to his
Disquisitiones Arithmeticae). The
period lattices are of a very special form, being proportional to the
Gaussian integers. For this reason the case of elliptic functions with
complex multiplication by square root of minus one| is called the
lemniscatic case in some sources. Using the elliptic integral :\operatorname{arcsl}x \stackrel{\text{def}}{{}={}} \int_0^x\frac{dt}{\sqrt{1-t^4}} the formula of the arc length can be given as :\begin{align} L &= 4a \int_{0}^1\frac{dt}{\sqrt{1-t^4}} = 4a\,\operatorname{arcsl}1 = 2\varpi a \\[6pt] &= \frac{\Gamma (1/4)^2}{\sqrt\pi}\,c =\frac{2\pi}{\operatorname{M}(1,1/\sqrt{2})}c\approx 7{.}416 \cdot c \end{align} where c and a = \sqrt{2}c are defined as above, \varpi = 2 \operatorname{arcsl}{1} is the
lemniscate constant, \Gamma is the
gamma function and \operatorname{M} is the
arithmetic–geometric mean. ==Angles==