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    Re: Interpolation of Meridional Part Table
    From: Andrés Ruiz
    Date: 2009 Mar 25, 13:47 +0100

    Three members of navlist have contacted with me off-line asking information.

    As I think this information might be of interest, here it is.

     

    The Meridional Parts can be calculated like this:

    Fi = latitude

    a = main axis

    Flattening: f=1-b/a

    Eccentricity: eoe = sqrt(2.0*f-SQ(f));

    Put the values on this formula, and you obtain the values.

    M1 = log(10)*log10(tan( 45.0+fi/2.0) );

    M2 = SQ( eoe )*sin( fi );

    M3 = pow( eoe, 4 )/3.0*pow( sin( fi ), 3);

    M4 = pow( eoe, 6 )/5.0*pow( sin( fi ), 5);

    M = a*(M1-M2-M3-M4)

    Values for "a" in nautical miles, and "f" for various Earth models:

    ·         BOWDITCH   21600.0/(2.0*PI), 1.0/298.26

    ·         WGS84      6378137.0/1852.0, 1.0/298.257223563

    ·         WGS72      6378135.0/1852.0, 1.0/298.26

    ·         ESFERA     21600.0/(2.0*PI), 0

    ·         NAD83      6378137.0/1852.0, 1/298.257222100880

    ·         GRS80       NAD83

    ·         EUROPE1950 6378388.0/1852.0, 1/297.0

    If a spherical-Earth model is used, then the to axis are equal: a=b, and f=0, eoe = 0

     

    More information at my web site: “The Sailings” paper.

     

    You can see that BOWDITCH use "a" for "f" spherical model and f for the WGS72. This is the error of concept.

     

    Andrés Ruiz

    Navigational Algorithms

    http://www.geocities.com/andresruizgonzalez

     


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