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Chapter 4: Geometry

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and the positive polar axis, and the angle (azimuth) between the initial ray and the<br />

projection of ÇÈ to the equatorial plane. See Figure 4.32. As in the case of polar<br />

and cylindrical coordinates, is only defined up to multiples of ¿¼ Æ , and likewise .<br />

Usually is assigned a value between ¼ and ½¼ Æ , but values of between ½¼ Æ and<br />

¿¼ Æ can also be used; the triples ´ µ and ´ ¿¼ Æ ½¼ Æ · µ represent the<br />

same point. Similarly, one can extend to negative values; the triples ´ µ and<br />

´ ½¼ Æ ½¼ Æ · µ represent the same point.<br />

FIGURE 4.32<br />

A set of spherical coordinates for È is ´ µ ´½¼ ¼ Æ ¿¼ Æ µ.<br />

<br />

<br />

È<br />

<br />

FIGURE 4.33<br />

Standard relations between Cartesian, cylindrical, and spherical coordinate systems. The<br />

origin is the same for all three. The positive Þ-axes of the Cartesian and cylindrical systems<br />

coincide with the positive polar axis of the spherical system. The initial rays of the cylindrical<br />

and spherical systems coincide with the positive Ü-axis of the Cartesian system, and the rays<br />

¼ Æ coincide with the positive Ý-axis.<br />

Þ<br />

<br />

<br />

È<br />

Ü<br />

Ý<br />

Ö<br />

<br />

© 2003 by CRC Press LLC

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