Polar distance (astronomy)
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In the celestial equatorial coordinate system Σ(α, δ) in astronomy, polar distance (PD) is an angular distance of a celestial object on its meridian measured from the celestial pole, similar to the way declination (dec, δ) is measured from the celestial equator.[1]
Definition
[edit]
Polar distance in celestial navigation is the angle between the pole and the position of body on its declination.[2]
Referring to diagram:
P- Pole, WQE- Equator, Z - Zenith of observer,
Y- Lower meridian passage of body
X- Upper meridian passage of body
Here body will be on declination circle (XY). The distance between PY or PX will be the Polar distance of the body.
NP=ZQ=Latitude of observer
NY and NX will be the True altitude of body at that instant.
Polar distance (PD) = 90° ± δ
Polar distances are expressed in degrees and cannot exceed 180° in magnitude. An object on the celestial equator has a PD of 90°.
Polar distance is affected by the precession of the equinoxes.
If the polar distance of the Sun is equal to the observer's latitude, the shadow path of a gnomon's tip on a sundial will be a parabola; at higher latitudes it will be an ellipse and lower, a hyperbola.
References
[edit]- ^ Main, Robert (1852). Rudimentary Astronomy. John Weale. p. 15. Retrieved 4 June 2025.
- ^ Stebbing, Frank Cole (1896). Navigation and Nautical Astronomy. Macmillan and Company. p. 81. Retrieved 4 June 2025.