Jump to content

Zenith: Difference between revisions

From Wikipedia, the free encyclopedia
Content deleted Content added
restored origin section
Line 4: Line 4:
For reference, the vertical direction at the given location and pointing in the same sense as the gravitational force is called the [[nadir]].
For reference, the vertical direction at the given location and pointing in the same sense as the gravitational force is called the [[nadir]].


'''Bold text'''''Italic text''JESUS IS THE WAY THE TRUTH AND THE LIFE...ALL HAVE SINNED AND COME SHORT OF THE GLORY OF GO AND HE IS JUST TO FOR GIVE USE
==Origin==
REPENT
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).
AND COME TO BETHEL WORLD OUTREACH ON GERGIA AVE.
IN SILVER SPRING


==Relevance and use==
==Relevance and use==

Revision as of 15:43, 11 November 2006

For other uses, see Zenith (disambiguation).

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.

Bold textItalic textJESUS IS THE WAY THE TRUTH AND THE LIFE...ALL HAVE SINNED AND COME SHORT OF THE GLORY OF GO AND HE IS JUST TO FOR GIVE USE REPENT AND COME TO BETHEL WORLD OUTREACH ON GERGIA AVE. IN SILVER SPRING

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 Moon and solar tides).

See also

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.