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Astronomy Principles and Practice Fourth Edition.pdf

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160 Geocentric planetary phenomena<br />

Figure 12.9. Superior planet at a stationary point.<br />

or<br />

cos(θ + φ) = V P<br />

cos φ. (12.6)<br />

V ⊕<br />

Now in any plane triangle XYZ with sides x, y, z <strong>and</strong> opposite angles X, Y , Z,wehave<br />

x = y cos Z + z cos Y.<br />

Applying this well-known formula to △SEP, we may write<br />

SP = PEcos φ + SE cos θ<br />

i.e.<br />

b = PEcos φ + a cos θ. (12.7)<br />

Applying it again to △SEP, we obtain<br />

SE = SP cos θ + PEcos SEP<br />

or<br />

a = b cos θ − PEcos(θ + φ) (12.8)<br />

since SEP = 180 − (θ + φ).<br />

Equations (12.7) <strong>and</strong> (12.8) give<br />

b − a cos θ = PEcos φ<br />

b cos θ − a = PEcos(θ + φ)<br />

so that<br />

b − a cos θ<br />

b cos θ − a = cos φ<br />

cos(θ + φ) . (12.9)

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