
Diagram showing the relationship between the Zenith, the
Nadir, and different types of
Horizon. Note that the Zenith is opposite the Nadir.
In broad terms, the 'zenith' is the direction pointing directly ''above'' a particular location (
perpendicular,
orthogonal). Since the concept of ''being above'' is itself somewhat vague, scientists define the zenith in more rigorous terms. Specifically, in
astronomy,
geophysics and related sciences (e.g.,
meteorology), the zenith at a given point is the local
vertical direction pointing away from direction of the force of
gravity at that location.
For reference, the vertical direction at the given location and pointing in the same sense as the gravitational force is called the
nadir.
Origin
Zenith derives from the inaccurate reading of the Arabic word ''samt'' (path), pronounced ''sent'', by scribes in the Middle Ages (during the 14th century), in the expression ''samt arrâs'' (path above the head).
Relevance and use
The zenith is used in the following scientific contexts:
★ It serves as the direction of reference for measuring the 'zenith angle', which is the angular distance between a direction of interest (e.g., a star) and the local zenith, relative to the point for which the zenith is defined.
★ It defines one of the axes of the
horizontal coordinate system in astronomy.
Discussion
★ The zenith directions corresponding to two different locations (not on the same vertical direction) are divergent.
★ Strictly speaking, the zenith is only 'approximatively' contained in the local
meridian plane because the latter is defined in terms of the rotational characteristics of the celestial body, not in terms of its gravitational field. The two coincide only for a perfectly rotationally symmetric body. On Earth, the axis of rotation is not fixed with respect to the planet (for example due to constant displacements of its fluid components) so that the local
vertical direction, as defined by the gravity field, is itself changing direction in time (for instance due to lunar and solar
tides).

Only in the tropics that it is possible for the
Sun to be at Zenith.
See also
★
Zenith distance
★
Geodesy
★
History of geodesy
★
Vertical deflection
★
Nadir
★
Midheaven
References
★ Huschke, Ralph E. (1959) ''Glossary of Meteorology'', American Meteorological Society, Boston, Second printing-1970.
★ McIntosh, D. H. (1972) ''Meteorological Glossary'', Her Majesty's Stationery Office, Met. O. 842, A.P. 897, 319 p.
★ Picoche, J. (1992) ''Dictionnaire Etymologique du Français'', Le Robert, Paris, ISBN 2-85036-458-4.