420 CHAPTER 10 • CONFORMAL MAPPING
y
2
(a)
w =sinz
-----+
x
t = 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.
v
u
(b)
We now eliminate x from the equations by squaring and using the trigonometric
identity 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 the
points (± 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 equation
x + iy = sinw = sinucosh v + icosusinhv (10-25)