A system of curvilinear coordinates. There are several different conventions for the orientation and designation of these coordinates.
Arfken (1970) defines coordinates such that
(1)
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(2)
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(3)
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In this work, following Morse and Feshbach (1953), the coordinates are used instead. In this convention, the traces of
the coordinate surfaces of the
-plane are confocal parabolas
with a common axis. The
curves open into the negative x-axis; the
curves open into the positive x-axis. The
and
curves intersect along the
y-axis.
(4)
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(5)
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(6)
|
where ,
,
and
.
The scale factors are
(7)
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(8)
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(9)
|
(10)
|
The Helmholtz differential equation is separable in parabolic cylindrical coordinates.