420 CHAPTER 10 • CONFORMAL MAPPING
y2(a)w =sinz
-----+xt = Arcsin w
~Figure 1 0.17 The transformation w = sin z.
for -; < x < j. We rewrite them as
. u d v
smx = -COS 1 l b an cosx = SI "nhb.
vu(b)We now eliminate x from the equations by squaring and using the trigonometricidentity sin^2 x + cos^2 x = 1. The result is the single equation
u2 v2
--+--=l.
cosh^2 b sinh^2 b(10-24)The curve given by Equation ( 10 -24) is identified as an ellipse in the uv plane
that passes through the points (± coshb,O) and (0,±sinhb) and has foci at thepoints (± 1,0). Therefore, if b > 0, then v = cosxsinhb > 0, and the image of
the horizontal segment is the portion of the ellipse given by Equation ( 10 -24)
that lies in the upper half-plane Im ( w) > 0. If b < 0, then it is the portion that
lies in t he lower half-plane. The images of several segments are shown in Figure
10. 17 (b). •10.4.1 The Complex Arcsine Function
We now develop explicit formulas for the real and imaginary parts of the principal
value of the arcsine function w = f (z) = Arcsinz. We use this mapping to solve
problems involving steady temperatures and ideal fluid flow in Section 11.7. The
mapping is found by solving t he equationx + iy = sinw = sinucosh v + icosusinhv (10-25)
