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A Community Devoted to the Preservation and Practice of Celestial Navigation and Other Methods of Traditional Wayfinding
Re: Advancing a position circle. was : [NAV-L] Position from crossing two circles
From: Andr�s Ruiz
Date: 2006 Jun 16, 13:58 +0200
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 ... ....