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    Re: Advancing a position circle. was : [NAV-L] Position from crossing two circles
    From: Andr�s Ruiz
    Date: 2006 Jun 16, 13:58 +0200

    The following text is extract of:
    
    Advancing Celestial Circles of Position
    THOMAS R. METCALF
    Institute for Astronomy, University of Hawaii
    
    ABSTRACT
    This paper presents rigorous equations, useful with computer reduction of 
    celestial sights, which correct the Greenwich Hour Angle and declination of a 
    celestial body for the motion of a vessel. Advancing a circle of position in 
    this way maintains the relationship between the geographical position of the 
    body and the vessel, and hence is the best method for advancing an 
    observation.
    
    INTRODUCTON
    When computing a running fix without the aid of a computer, one generally 
    proceeds graphically by advancing a line of position (LOP) on a chart. To the 
    extent that an LOP is a good approximation to the true circle of position, 
    this technique works well. However, the graphical approach does not yield an 
    efficient algorithm when calculating a running fix with a computer. Instead, 
    to allow for the motion of the observer, the program adjusts the 
    observations, not the LOP directly.
    The simplest method of advancing an observation with a computer involves a 
    correction to the observed altitude of a celestial body [1, 2]. However, this 
    is clearly an approximation since it may alter the direction of the LOP, 
    particularly for observations of bodies near the zenith. To advance the 
    entire circle of position, and hence maintain the orientation of the LOP, one 
    corrects the Greenwich Hour Angle (GHA) and declination of the observed body. 
    By correcting the GHA and declination rather than the altitude, the circle of 
    position is "dragged" along with the vessel, making the correction exact. An 
    approximate technique for advancing the GETA and declination that is adequate 
    for almost ah situations encountered in navigation is presented in [1]. 
    However, a rigorous formulation is not much more demanding computationally 
    and, with the advent of the handheld computer, may be of interest.
    Table 1 indicates typical errors incurred when using the approximate 
    techniques discussed aboye to advance the observation of a body near the 
    zenith (85?17'). The first column gives the distance traveled from the 
    starting point (45? N, 30.3? W). The second column shows the error in the 
    geographical position (GP) of the fictitious body when the GHA and 
    declination are advanced using the approximate formulae given in [1]. The 
    error in a derived position could be substantially larger for LOPs that cross 
    at small angles, as in the case of multiple sights of a single body over a 
    relatively short period of time [3, 4]. The third column shows the error in 
    the orientation of an LOP computed by altering the observed altitude of the 
    body to correct for observer motion. Again, the error in the derived position 
    could be considerable when the LOPs intersect at small angles.
    
    METHOD
    Since the geographical position of the observed body is not necessarily near 
    the vessel, the correction cannot be made by simply moving the GP the same 
    distance along the same course as the vessel's motion. Instead, the 
    coordinate system defining GHA and declination is mathematically rotated by 
    an amount equal to the vessel's change in latitude and longitude, since any 
    rotation will preserve the relative position of the GP and the vessel. In 
    other words, rather than treating the vessel as moving over a fixed surface, 
    the vessel and the GP are considered fixed, with the earth moving underneath 
    them in such a way that the vessel begins and ends at the appropriate places. 
    The final position of the GP after this rotation is the advanced GP we seek.
    The usual convention is to describe the GP with two angles: the GHA and the 
    declination. However, the rotation takes a simpler form if the GP is 
    represented as a vector directed from the center of the earth to the actual 
    GP on the surface. With the axis of the rotation represented vectorally by 
    ...
    ....
    
    
    

       
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