⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂
∂
+
∂
∂
−
⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂
∂
+
∂
∂
=
∂
∂
+
∂
∂
y
u
x
v
vu
y
V
v
x
V
u
2
1
y
v
v
x
u
u
22
22
Using the definition of velocity potential, the above equation becomes
⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂∂
∂
∂
∂
∂
∂
−
⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂
∂
∂
∂
+
∂
∂
∂
∂
=
∂
∂
⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂
∂
+
∂
∂
⎟
⎟
⎠
⎞
⎜
⎜
⎝
⎛
∂
∂
yx
φ
2
y
φ
x
φ
y
V
y
φ
x
V
x
φ
2
1
y
φ
y
φ
x
φ
x
φ2
22
2
2
2
2
2
2
Substitution of this into the right hand side of the Eq. (3) then yields Eq. (1).
Problem 2. – Show that polar velocity components vr and vθ are related to the Cartesian
velocity components u and v by
θ+θ−=
θcosvsinuv
sinvcosuvr
Find the inverse of these, i.e., develop expressions for u = u (vr, vθ) and v = v (vr, vθ).
Consider the following figure
where r
e
ˆ and θ
e
ˆ are the unit normal vectors of the polar coordinate system. These unit
vectors are related to the Cartesian unit vectors, i
ˆand j
ˆ, through a counterclockwise
rotation of angle θ. In other words
⎥
⎦
⎢
⎣
⎥
⎦
⎢
⎣
θθ−
=
⎥
⎦
⎢
⎣
θj
ˆ
cossin
e
ˆ
Now consider the velocity vector expressed in both coordinate systems
Substituting for the polar unit vectors from Eq. (1) in the above yields
From Gas Dynamics, Third Edition, by James E. John and Theo G. Keith. ISBN 0-13-120668-0. © 2006 Pearson Education, Inc.,
Upper Saddle River, NJ. All rights reserved. This material is protected under all copyright laws as they currently exist. No Portion of
this material may be reproduced, in any form or by any means, without permission in writing from the publisher.