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Horizon system of coordinates
 

Horizon system of coordinates

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    Horizon system of coordinates Horizon system of coordinates Presentation Transcript

    • Horizon System of Coordinates
      Group 4:
      “The Celestials”
    • Horizon
      The horizon  is  a  plane  through  the  observer’s position  that  is  perpendicular  to  the  direction  of  gravity at that point and that intercepts the celestial sphere in a great  circle.
       The  direction  of  gravity,  commonly  called the direction of the plumb line, does not necessarily pass through  the  earth’s  center.  The  horizon  plane  is considered tangent to the surface of the earth at the observer’s  position  For  most  star  observations,  the distance from this plane to the center of the earth is too small  to  affect  the  computations.
    • Visible Horizon
      A projection of the local horizon outward to intersect with the celestial sphere. Also known as the apparent horizon.
    • Astronomical horizon (or sensible horizon)
      The great circle formed by the intersection of the celestial sphere with a plane perpendicular to the line from an observer to the zenith; in other words, the great circle whose poles are the nadir and zenith.
    • Zenith
      In general terms, the zenith is the direction pointing directly "above" a particular location; that is, it is one of two vertical directions at the location, orthogonal to a horizontal flat surface there.
    • The zenith is used in the following scientific contexts:
      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.
      Defines one of the axes of the horizontal coordinate system in astronomy.
    • Nadir
      The nadir (from Arabic nadhir, "opposite") is the direction pointing directly below a particular location.
    • Rational or Celestial Horizon
      It is a plane passing through the center of the Earth and parallel to the sensible horizon.
    • Geoid
      The geoid is that equipotentialsurface which would coincide exactly with the mean ocean surface of the Earth, if the oceans were in equilibrium, at rest (relative to the rotating Earth), and extended through the continents (such as with very narrow canals).
    • Geoidal Horizon
      Is an imaginary plane parallel to the sensible horizon, but through the point on the geoid (the sea level surface of the Earth) vertically below the observer.
    • Geometrical Horizon
      It is an imaginary plane parallel to the sensible horizon, but through the point on the geoid (the sea level surface of the Earth) vertically below the observer.
    • This system is based upon the celestial horizon as the primary great circle and a series of secondary vertical circles which are great circles through the zenith and nadir of the observer and hence perpendicular to his horizon (Figure A).
    • Figure A
    • As shown in Figure B, altitude is angular distance above the horizon. It is measured along a vertical circle, from 0° at the horizon through 90° at the zenith.
    • Figure B
    • Thank you for listening…
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    • Reporters:
      Muring, Mart Angelo
      Pendon, Vincent
      Ramos, Davey Boy
      Selera, Carlo Martin