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Thread: How far away is the horizon??

  1. #31
    slug_burner is offline TopicToaster Gold Subscriber
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    Quote Originally Posted by CraigE View Post
    The main factor is m above true sea level. Standing at the waters edge is not necessarily true sea level. Dose get very confusing unless you know exactly how far above sea level you are.
    For searching we work on a few generic distances.
    Inland more than 60kms, usually you are over 100m above sea level, so provided you can see the horizon to start with we work on 20 mile.
    If on a hill, you can see significantly more.
    In a plane this increases vastly.
    However for us the horizon is only a reference point and does not have a lot of values apart from looking for signals such as smoke or mirror refraction.
    At the beach standing at the high water mark we generally work at a height above sea level of around 5 metres. Then things like swell also come into play as well as clarity, sea mist, cloud, haze, glare etc.
    Maximum visible distance to the horizon is calculated on an ideal day.
    Craig are you saying that on Lake Eyre at approximately 15 m (49 ft) below sea level the horizon is at a different distance to that at Lake Titicaca with a surface elevation of 3,812 m?

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    Oooooooh!!! My brain hurts.

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    Quote Originally Posted by slug_burner View Post
    Craig are you saying that on Lake Eyre at approximately 15 m (49 ft) below sea level the horizon is at a different distance to that at Lake Titicaca with a surface elevation of 3,812 m?
    I would imagine it's not that straightforward. Distance to horizon equations are all based on what's known as the Tangent Secant Theorem, and therefore count on the horizon being at sea level. Both lakes being inland lakes, far from the sea, the distance to the horizon would be completely dependant on the terrain surrounding the lakes.

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    what about if your standing on the edge of a black hole looking in how far to the horizin then

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    You would be stretched so much by the warped space time that the electrical impulses traveling along your optic nerve would never reach your brain....

  6. #36
    slug_burner is offline TopicToaster Gold Subscriber
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    Quote Originally Posted by slug_burner View Post
    Craig are you saying that on Lake Eyre at approximately 15 m (49 ft) below sea level the horizon is at a different distance to that at Lake Titicaca with a surface elevation of 3,812 m?
    Quote Originally Posted by mike_ie
    Distance to horizon equations are all based on what's known as the Tangent Secant Theorem, and therefore count on the horizon being at sea level.
    So given that at best we are approximating the earth with a sphere of approximate diameter of 12756.2 km the Tangent Secant Theorem gives us a horizon for an observation point of 2m above the surface of Kati Thanda – Lake Eyre of 5050.977m and on Lake Titicaca 5051.735. For the 0.75m difference in 5km it is hardly worth the effort of doing the calculations, the error in the approximation of the earth to a sphere probably accounts for any error introduced by the altitude of the surface for which you are working out the distance to the horizon. But according to the theorem yes there is a difference

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    Quote Originally Posted by slug_burner View Post
    So given that at best we are approximating the earth with a sphere of approximate diameter of 12756.2 km the Tangent Secant Theorem gives us a horizon for an observation point of 2m above the surface of Kati Thanda – Lake Eyre of 5050.977m and on Lake Titicaca 5051.735. For the 0.75m difference in 5km it is hardly worth the effort of doing the calculations, the error in the approximation of the earth to a sphere probably accounts for any error introduced by the altitude of the surface for which you are working out the distance to the horizon. But according to the theorem yes there is a difference
    As has been said the calculations are based on visible horizon, with no interference (mountains, trees, buildings etc etc). Hence why if we ever need to see the horizon you find a high point with unobstructed views. With GPS it is fairly easy as you will have your elevation and some GPS units or weather units will even calculate your distance to horizon. Generally we will only use the horizon for locating incoming aircraft, ships - boats etc. Fairly mute now with the advent of GPS for anything other than spotting.
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    We have that F bisects AC and that CD is added to it.
    Apply Square of Sum less Square:

    AD⋅DC+FC^2=FD
    But FC=FB and so:
    AD⋅DC+FB^2=FD^2

    Applying Pythagoras's Theorem, FD^2=FB^2+DB^2 therefore:

    AD⋅DC+FB^2=FB^2+DB^2
    AD⋅DC=DB^2
    DB = sqrt (AD.DC)

    Make the following substitutions:
    d = DB = distance to the horizon
    D = AC = diameter of the Earth
    h = DC = height of the observer above sea level
    D+h = AD = diameter of the Earth plus height of the observer above sea level

    d = sqrt (h(D+h))

    PERSON STANDING AT LAKE TITICACA:
    D = 12756200m
    h = 3812m

    d = sqrt(48641165744)
    d = 220547.42m or 22.5km


    PERSON STANDING AT THE SEA SHORE
    D = 12756200m
    h = 2m

    d = sqrt (2(12756200+2)
    d = sqrt (25512404)
    d = 5050.98m, or 5.05km

    ...so yes, there's a big difference in what a person standing at Lake Titicaca can see, vs a person standing on the beach.

    Below sea level values throw the formula into disarray, due to having to get the square root of a negative value, but it applies to all values above zero.

    Of course, this is the theoretical, and assumes that the horizon you are looking at is at sea level. Easiest real world scenario to prove effects of terrain - stand on a beach that has a mountain range behind you. Looking out to sea, the horizon id about 5km away. Looking behind you, the horizon i wherever the top of the mountain is, probably 6-700m away....

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    Quote Originally Posted by mike_ie View Post


    We have that F bisects AC and that CD is added to it.
    Apply Square of Sum less Square:

    AD⋅DC+FC^2=FD
    But FC=FB and so:
    AD⋅DC+FB^2=FD^2

    Applying Pythagoras's Theorem, FD^2=FB^2+DB^2 therefore:

    AD⋅DC+FB^2=FB^2+DB^2
    AD⋅DC=DB^2
    DB = sqrt (AD.DC)

    Make the following substitutions:
    d = DB = distance to the horizon
    D = AC = diameter of the Earth
    h = DC = height of the observer above sea level
    D+h = AD = diameter of the Earth plus height of the observer above sea level

    d = sqrt (h(D+h))

    PERSON STANDING AT LAKE TITICACA:
    D = 12756200m
    h = 3812m

    d = sqrt(48641165744)
    d = 220547.42m or 22.5km


    PERSON STANDING AT THE SEA SHORE
    D = 12756200m
    h = 2m

    d = sqrt (2(12756200+2)
    d = sqrt (25512404)
    d = 5050.98m, or 5.05km


    Below sea level values throw the formula into disarray, due to having to get the square root of a negative value, but it applies to all values above zero.

    Of course, this is the theoretical, and assumes that the horizon you are looking at is at sea level. Easiest real world scenario to prove effects of terrain - stand on a beach that has a mountain range behind you. Looking out to sea, the horizon id about 5km away. Looking behind you, the horizon i wherever the top of the mountain is, probably 6-700m away....
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  10. #40
    slug_burner is offline TopicToaster Gold Subscriber
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    Quote Originally Posted by mike_ie View Post


    We have that F bisects AC and that CD is added to it.
    Apply Square of Sum less Square:

    AD⋅DC+FC^2=FD
    But FC=FB and so:
    AD⋅DC+FB^2=FD^2

    Applying Pythagoras's Theorem, FD^2=FB^2+DB^2 therefore:

    AD⋅DC+FB^2=FB^2+DB^2
    AD⋅DC=DB^2
    DB = sqrt (AD.DC)

    Make the following substitutions:
    d = DB = distance to the horizon
    D = AC = diameter of the Earth
    h = DC = height of the observer above sea level
    D+h = AD = diameter of the Earth plus height of the observer above sea level

    d = sqrt (h(D+h))

    PERSON STANDING AT LAKE TITICACA:
    D = 12756200m
    h = 3812m

    d = sqrt(48641165744)
    d = 220547.42m or 22.5km


    PERSON STANDING AT THE SEA SHORE
    D = 12756200m
    h = 2m

    d = sqrt (2(12756200+2)
    d = sqrt (25512404)
    d = 5050.98m, or 5.05km

    ...so yes, there's a big difference in what a person standing at Lake Titicaca can see, vs a person standing on the beach.

    Below sea level values throw the formula into disarray, due to having to get the square root of a negative value, but it applies to all values above zero.

    Of course, this is the theoretical, and assumes that the horizon you are looking at is at sea level. Easiest real world scenario to prove effects of terrain - stand on a beach that has a mountain range behind you. Looking out to sea, the horizon id about 5km away. Looking behind you, the horizon i wherever the top of the mountain is, probably 6-700m away....
    Mike,

    I think you have made an error. On a plane or lake some distance above or below sea level both point B and C are raised or lowered by the altitude (3812m for Titicaca and -15 for Kati Thanda – Lake Eyre and DC is only 2m (not 3812+2 or -15+2, otherwise the water in the lake would all run down one end real quick).

    Above or below sea level does not matter. You have to calculate a new value of AC allowing for the altitude. Just use DB^2=AD.DC.

    I think what you calculated when you got 22.5km to the horizon is the equivalent of the horizon for when you are standing on a 3812m mountain at the beach looking out over the sea.

    Hope I am not keeping you from getting your defender going again!

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