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)
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where , , and . The scale factors are
(7)
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(8)
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(9)
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(10)
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The Helmholtz differential equation is separable in parabolic cylindrical coordinates.