Part 1:  Change of Variable into Polar Coordinates

We can also apply the change of variable formula to the polar coordinate transformation

x = rcos( q) ,    y = rsin( q)
However, due to the importance of polar coordinates, we derive its change of variable formula more rigorously.

To begin with, the Jacobian determinant is
 ( x,y)
( r,q)
= ê
ê
ê
cos( q)
sin( q)
-rsin( q)
rcos( q)
ê
ê
ê
= rcos2( q) +rsin2( q) = r
As a result, the area differential for polar coordinates is
dA = ê
ê
 ( x,y)
( r,q)
ê
ê
drdq = r dr dq

Let us consider now the polar region S defined by
q = a,q = b,r = g( q) ,r = f( q)
where f( q) and g( q) are contained in [ p,q] for all q in [ a,b] . If q0,¼,qm is an h-fine partition of [a,b] and r0,¼,rn is an h-fine partition of [ p,q] , then the image of [ a,b]×[ p,q] is a partition of the image of the region with near parallelograms whose areas are denoted by DAjk:

Since the area differential is dA = rdrdq, the area of the "near parallelogram" is approximately

DAjk » rjDrjDqj
so that if xjk = rjcos( qk) and yjk = rjsin( qk) , then

lim
h® 0 
n
å
j = 1 
m
å
k = 1 
f(xjk,yjk) DAjk =
lim
h®0 
n
å
j = 1 
m
å
k = 1 
f( rjcos( qk) ,rjsin( qk) ) rjDrjDqj

Writing each of these limits as double integrals results in the formula for change of variable in polar coordinates:
f( x,y) dA = ó
õ
b

a 
ó
õ
f( q)

g(q)  
f( rcos(q), rsin(q) )   rdrdq
(1)
To aid in the use of (1), let us notice that if p is constant, then r = p is a circle of radius p centered at the origin in the xy-plane, while if a is constant, then q = a is a ray at angle a beginning at the origin of the xy-plane.

Polar coordinates for the origin are r = 0 for every value of q.       

 

EXAMPLE 1    Use (1) to evaluate
ó
õ
1

0 
ó
õ
Ö
2-x2
( x2+y2) dydx
x
Solution: To do so, we transform the iterated integral into a double integral
ó
õ
1

0 
ó
õ
Ö
2-x2
( x2+y2)dydx =   ( x2+y2) dA
x
where R is a sector of a circle with radius Ö2. In polar coordinates, R is the region between r = 0 and r = Ö2 for q in [ p/4,p/2] :

Since r2 = x2+y2, the double integral thus becomes

 ( x2+y2) dA =
ó
õ
p/2

p/4 
ó
õ
Ö2

0 
r2  rdrdq =
ó
õ
p/2

p/4 
ó
õ
Ö2

0 
r3  drdq
and the resulting iterated integral is then easily evaluated:
( x2+y2) dA =
ó
õ
p/2

p/4 
 r4
4
ê
ê
Ö2

0 
dq =
ó
õ
p/2

p/4 
dq =  p
4

               

Check your Reading: What does y = x, x > 0 correspond to in polar coordinates?