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    Re: Navigation exercise
    From: George Huxtable
    Date: 2008 May 25, 17:02 +0100

    Bill is worrying away at this question of the shape of the altitude curve of
    the Sun, around noon, and the effect on it of the speed and direction of the
    vessel.
    
    Let me take, first, his final question, which was-
    
    "What about east/west displacement if trying to determine longitude from
    LAN?", and will assume, for that purpose, that the ship has no motion in the
    North-South direction, but is travelling East-West only, and the Sun's
    decllination is unchanging, at a solstice..
    
    The moment of LAN (Local Apparent Noon) is when the Sun and the ship are on
    the same meridian. The Sun will always be crossing meridians, going
    Westward, at almost exactly 15 degrees per hour. The ship will be crossing
    meridians travelling much more slowly, at a few tens of minutes in an hour,
    perhaps in the same direction as the Sun, perhaps the opposite direction.
    The moment when they cross the same meridian will depend on that speed, so
    to calculate that moment you must take the speed into account, but the
    maximum height of the Sun will occur at that moment and will not depend on
    the speed of the vessel.  The only effect you would see, if you examined the
    curve of altitude against time more closely, was that it would be very
    slightly peakier, changing slightly faster with time if the vessel was
    travelling Eastward than vice versa. However, it would still have the same
    maximum value, at the same moment, of LAN. There would be no surprises.
    
    North-South travel, around noon, has a very different effect, the details of
    which Bill questions. Judging by his words, he finds it hard to accept that
    it can result in a symmetrical curve of altitude against time: symmetrical,
    not about noon, but about a moment displaced, earlier or later, in time.
    It's because of the way two quite different changes combine together.
    
    The speed, Northward or Southward, of a vessel, has a very similar but
    greater effect than the changing declination of the Sun (which can be up to
    1 knot at the equinoxes) So just let's consider a vessel moving Southward at
    say 10 knots, at Winter solstice, at a position of say 56 deg North. And
    let's make an enormous supposition, that at the moment of LAN, we could stop
    the rotation of the Earth. The Sun would then really "hang " in the sky,
    absolutely stationary. But to our observer on the Ship, not quite
    stationary. He would still be travelling Southward, toward the Sun, at 10
    arcminutes per hour, so to him the Sun would be slowly increasing in
    altitude, at that rate.
    
    Now put that picture to one side, and set the Earth rotating again. And now,
    take the vessel to be stationary. Now our observer sees a familiar curve:
    the Sun climbs, reaches a peak, then falls, quite symmetrically about LAN.
    Actually, near the peak, that's as close as you like to a parabolic curve,
    where the drop, from the peak value, changes with the square of the time
    from the peak.
    
    And now, in real life, we have to combine those two motions together, the
    symmetrical parabola with the steadily changing altitude, increasing at 10
    minutes an hour. And I suspect that the only way to convince Bill will be to
    persuade him to take a bit of graph paper and combine them for himself.
    
    As an example, let's take the ship approaching the Clyde in Winter, that I
    tried to get Frank to consider as a noon-longitude exercise (but he ducked).
    The noon Sun (neglecting corrections) would be at 10 deg 30' altitude.
    Before and after that moment, if the ship is stationary, it will be somewhat
    less. Here are some numbers.
    
    First column, time in minutes before and after LAN.
    Second column, Sun altitude with stationary observer.
    Third column, change in altitude due to observer's motion.
    Fourth column, combination of the two.
    
    time (min)     alt1           shift      sum
    LAN-20   10d 23.1     -3.3   10d 19.7
    LAN-15   10d 26.2    -2.5    10d 23.7
    LAN-10   10d 28.3    -1.7    10d 26.6
    LAN-5     10d 29.6    -0.8    10d 28.8
    LAN        10d 30.0      0.0    10d 30.0
    LAN+5    10d 29.6    +0.8   10d 30.4
    LAN+10  10d 28.3    +1.7   10d 30.0
    LAN+15  10d 26.2    +2.5   10d 28.7
    LAN+20  10d 23.1    +3.3   10d 26.4
    
    Anyone who cares to plot out the fourth column will find it to be just
    another parabola, perfectly symmetrical in itself, but with its centre of
    symmetry displaced to be about 5 minutes later than LAN. It also has a
    slightly higher peak value but not very significantly so, which allows an
    observer to take either the altitude at LAN, or the maximum altitude,
    without bothering much about the difference.
    
    But not so the difference in the timing of that central value, to anyone
    trying to use Frank's proposed method to find his longitude. The correction
    that has to be made for the ship's south-going speed of 10 knots is all of 5
    minutes of time, or 1.25 degrees of longitude, which has to accommodate the
    speed of the ship, any tidal current and any declination changes in the Sun
    position. With modern shipping commonly travelling at over 25 knots, it's
    obvious what an enormous correction this must be, and how precisely it would
    have to be made.
    
    And yet Frank is claiming that he can derive the central moment of that
    altitude curve, and then make that correction, to provide an overall error
    in the whole process of no more than 5 miles in longitude, which corresponds
    to 35 seconds of time. No wonder he is reluctant to disclose the details.
    
    George.
    
    contact George Huxtable at george@huxtable.u-net.com
    or at +44 1865 820222 (from UK, 01865 820222)
    or at 1 Sandy Lane, Southmoor, Abingdon, Oxon OX13 5HX, UK.
    
    
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