Curvature of the Horizon

  • #1
ScarBest
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TL;DR Summary
I request advice on where to publish a paper on calculating the curve of the horizon seen from various altitudes.
I'm writing a paper on how to calculate the visible curvature of the horizon for any given altitude. I'm considering attempting to have it published. I wonder if anyone could suggest a publication that might be interested in such a paper. If this isn't the best forum for this request, please suggest another. Thank you.
 
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  • #2
ScarBest said:
TL;DR Summary: I request advice on where to publish a paper on calculating the curve of the horizon seen from various altitudes.

I'm writing a paper on how to calculate the visible curvature of the horizon for any given altitude. I'm considering attempting to have it published. I wonder if anyone could suggest a publication that might be interested in such a paper. If this isn't the best forum for this request, please suggest another. Thank you.
https://en.wikipedia.org/wiki/Horizon
 
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  • #3
ScarBest said:
I wonder if anyone could suggest a publication that might be interested in such a paper.
The journal will depend on the application of your solution.
Have you done a literature search?
I think you will find that it has been published before.

The angular depression of the horizon, increases with altitude, and can be measured with a theodolite. The distance to the horizon is typically calculated for altitude, when range of visibility, range of radio communication, or RADAR coverage is being analysed.

When taking star sights with a sextant for astronomical navigation, angular depression of the horizon is estimated from tables.

How do you specify "curvature of the horizon"? Surely it is always a circle, 360°.
The horizon would have a radius of curvature, measured as an angle from the vertical, at the observer's altitude. Is that radius not simply 90°, minus the depression of the horizon?
 
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  • #4
Welcome to PF.

ScarBest said:
I'm considering attempting to have it published. I wonder if anyone could suggest a publication that might be interested in such a paper.
What journals are the papers in your References from? Typically you will be publishing in a journal that you read frequently, and has similar papers in it.
 
  • #5
Baluncore said:
The journal will depend on the application of your solution.
Have you done a literature search?
I think you will find that it has been published before.

The angular depression of the horizon, increases with altitude, and can be measured with a theodolite. The distance to the horizon is typically calculated for altitude, when range of visibility, range of radio communication, or RADAR coverage is being analysed.

When taking star sights with a sextant for astronomical navigation, angular depression of the horizon is estimated from tables.

How do you specify "curvature of the horizon"? Surely it is always a circle, 360°.
The horizon would have a radius of curvature, measured as an angle from the vertical, at the observer's altitude. Is that radius not simply 90°, minus the depression of the horizon?
I meant the curve that would be visible to the observer. At sea level, the horizon appears to be a straight line. From the International Space Station, there is an obvious curve visible. My paper shows how to calculate and graph the curve that would be visible to an observer at a given altitude.
 
  • #6
berkeman said:
Welcome to PF.


What journals are the papers in your References from? Typically you will be publishing in a journal that you read frequently, and has similar papers in it.
I'm not a professional scientist and I don't read journals. My calculations are a mathematical treatment that doesn't rely on the work of others, so I don't have any references.
 
  • #8
ScarBest said:
I'm not a professional scientist and I don't read journals.
But if you don't read journals and/or other references, how can you be sure your work is truly novel versus just rediscovering knowledge that is already well-known and discussed?
 
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  • #9
renormalize said:
But if you don't read journals and/or other references, how can you be sure your work is truly novel versus just rediscovering knowledge that is already well-known and discussed?
I don't know this. However, I have searched online and I've found nothing like it. If I were to submit it to a journal, the editor would know and inform me.
 
  • #10
ScarBest said:
I don't know this. However, I have searched online and I've found nothing like it. If I were to submit it to a journal, the editor would know and inform me.
I would expect a bright high school student to be able to calculate the distance to the horizon from a given altitude. What are you doing that is more than basic trigonometry?
 
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  • #11
PeroK said:
I would expect a bright high school student to be able to calculate the distance to the horizon from a given altitude. What are you doing that is more than basic trigonometry?
I'm not calculating the distance to the horizon. I'm calculating the curved shape of the horizon as it would appear to an observer. From sea level, the curve is imperceptible. From low earth orbit, it's obvious. I'm calculating and graphing the curve that would be seen from various altitudes.
 
  • #12
ScarBest said:
I'm calculating and graphing the curve that would be seen from various altitudes.
Are you calculating that for a spherical Earth, or for an oblate spheroid, such as the WGS84 standard used by GPS positioning system ?
 
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  • #13
ScarBest said:
I'm not calculating the distance to the horizon. I'm calculating the curved shape of the horizon as it would appear to an observer. From sea level, the curve is imperceptible. From low earth orbit, it's obvious. I'm calculating and graphing the curve that would be seen from various altitudes.
It's a similar calculation. The curvature of a circle is 1/radius. It's still basic trig.
 
  • #14
I was thinking about what you would measure from the vantage point above the surface of the Earth. Essentially, you are looking down on a circle from some point above the centre of the circle. You could measure the angle below the horizontal to the horizon. Let's call that ##\gamma##. As you scan the horizon, ##\gamma## is constant. Without measuring distances, that seems to be the key measurable quantity.

In fact, looking at the Wikipedia page, the zenith angle is defined as ##\gamma + \pi/2##.

An accurate measurement of ##\gamma## would allow us to calculate the radius of the Earth, as:
$$\cos \gamma = \frac{R}{R+h}$$That's as far as high-school mathematics can take us.

However, the Wikipedia page continues with calculations involving the effect of atmospheric refraction:

https://en.wikipedia.org/wiki/Horizon#Effect_of_atmospheric_refraction

Even that would be seen by a journal editor as long-established calculations. To get something published on this, we would need something very special indeed!
 
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  • #15
Baluncore said:
Are you calculating that for a spherical Earth, or for an oblate spheroid, such as the WGS84 standard used by GPS positioning system ?
For a spherical earth. Calculating for an oblate spheroid would introduce considerable complexity, and since the earth is so close to being spherical, I don't think there would be any noticeable difference visually.
 
  • #16
PeroK said:
It's a similar calculation. The curvature of a circle is 1/radius. It's still basic trig.
When I talk about the curvature of the horizon, I'm not talking about the mathematical definition of curvature. I'm talking about the curved shape that the horizon would take as viewed by an observer. Since the radius of the horizon circle gets smaller the lower the altitude, your interpretation would cause the horizon to appear more curved the lower you are; the opposite is true. When an observer is close to the earth's surface, and the observer directs his attention at the point of the horizon in front of him, he is seeing a greatly foreshortened view of the horizon circle, causing it to appear as a highly eccentric ellipse, thus causing it to seem as if it had no curve at all. As you go higher, the angle to the horizon circle increases, reducing the foreshortening and increasing the amount of the circle you see in your field of vision, thus causing the horizon to appear more curved. I'm talking about the *visual* curve of the horizon - the actual shape that would be seen by an observer.
 
  • #17
ScarBest said:
As you go higher, the angle to the horizon circle increases, reducing the foreshortening and increasing the amount of the circle you see in your field of vision, thus causing the horizon to appear more curved.
Who defines your angular field of vision?
How is field of vision specified?
 
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  • #18
ScarBest said:
When I talk about the curvature of the horizon, I'm not talking about the mathematical definition of curvature. I'm talking about the curved shape that the horizon would take as viewed by an observer.
I get that:

PeroK said:
I was thinking about what you would measure from the vantage point above the surface of the Earth. Essentially, you are looking down on a circle from some point above the centre of the circle. You could measure the angle below the horizontal to the horizon. Let's call that γ. As you scan the horizon, γ is constant. Without measuring distances, that seems to be the key measurable quantity.

In fact, looking at the Wikipedia page, the zenith angle is defined as γ+π/2.


ScarBest said:
Since the radius of the horizon circle gets smaller the lower the altitude, your interpretation would cause the horizon to appear more curved the lower you are; the opposite is true. When an observer is close to the earth's surface, and the observer directs his attention at the point of the horizon in front of him, he is seeing a greatly foreshortened view of the horizon circle, causing it to appear as a highly eccentric ellipse, thus causing it to seem as if it had no curve at all.
The horizon is a circle, although you are not at its centre, but above its centre. It can't be an ellipse, as all direction are equivalent.
ScarBest said:
As you go higher, the angle to the horizon circle increases, reducing the foreshortening and increasing the amount of the circle you see in your field of vision, thus causing the horizon to appear more curved. I'm talking about the *visual* curve of the horizon - the actual shape that would be seen by an observer.
That's all covered in my post above, and on the Wikipedia page.
 
  • #19
Baluncore said:
Who defines your angular field of vision?
How is field of vision specified?
That's a good question. How far one can see to the side when looking ahead is more a question of psychology than math or physics. I can calculate the shape of the curve at all peripheral angles up to a chosen limit. I've been using 45 degrees.
 
  • #20
ScarBest said:
That's a good question. How far one can see to the side when looking ahead is more a question of psychology than math or physics.
It's a question of angles. Unless you can measure the distance, angles are all you have. The zenith angle is the same in all directions.
ScarBest said:
I can calculate the shape of the curve at all peripheral angles up to a chosen limit. I've been using 45 degrees.
It's always a circle, viewed from a point above its centre.
 
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  • #21
At the surface the horizon looks flat because it covers half the sphere of vision; 180 degrees, so if you want radius it's 90 degrees. Once you calculate ##\gamma## then the radius is just 90 - ##\gamma##

This is just a more complex case of calculating the angular diameter of a celestial object where its 3d (sphere) size matters instead of just it's 2d diameter. ##\gamma## is the harder part but as said, not that hard.
 
  • #22
Ignoring atmospheric effects, one point you may be missing is that at sea level, the horizon appears as a straight line unless you realize that it surrounds you as you follow the line. Hence, you are in the center of a circle.

The same is true as you go higher in altitude, but it becomes slightly more curved until you begin to see a circle.
 
  • #23
I don't think OP is missing that, I think it's what they want to somehow quantify (which the math given so far pretty much already does).
 
  • #24
ScarBest said:
I don't know this. However, I have searched online and I've found nothing like it. If I were to submit it to a journal, the editor would know and inform me.
That attitude greatly disrespects journal editors and their referees. They aren't schoolteachers who critique and grade the solution to a student's homework problem. Editors rightly expect a submitter to be expert in their field and its literature. Otherwise, how can the submitter even judge whether their own work is novel and useful?
 
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  • #25
renormalize said:
That attitude greatly disrespects journal editors and their referees. They aren't schoolteachers who critique and grade the solution to a student's homework problem. Editors rightly expect a submitter to be expert in their field and its literature. Otherwise, how can the submitter even judge whether their own work is novel and useful?
The problem would fit better in the physics or mathematics homework forums on here.
 
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  • #26
Apologies if this has already been answered

ScarBest said:
TL;DR Summary:
...visible curvature...

Has anyone determined what this means, mathematically?

By visible, does that limit us to human eyes and brain power?: 180° field of view, & resolution.
If not, then mathematically, we should be able to determine that the earth is curved from anything above zero altitude. A somewhat trivial problem which I solved several years ago.

If we are limited to human eyes and brains, then google claims we have to be at an altitude of 35000 feet to 'visually' see it.

In any event, I'm confused how to measure 'visible curvature' in other than in binary terms: 'Yes' it's curved, and 'No' it's not.

A quick search finds that wiki's circle definition of curvature yields 'curvature = 1/radius'
which indicates 3 terms:
1/(radius --> 0) = ∞
1/(0 > radius > ∞) = curved
1/∞ = not curved

Which strikes me as stupid, as changing how one measures the radius changes the curvature.
 
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  • #27
The observer is at the apex of the tangent cone surface. The radius of the horizon is the half-angle of the cone, measured by the observer, as the angle from the axis of the cone to the tangent horizon. The curvature of the horizon is (1 / radius angle), specified in units of inverse angle.
 
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  • #28
Baluncore said:
The observer is at the apex of the tangent cone surface. The radius of the horizon is the half-angle of the cone, measured by the observer, as the angle from the axis of the cone to the tangent horizon. The curvature of the horizon is (1 / radius angle), specified in units of inverse angle.
66 years around the sun, and I have zero recollection of a single conversation regarding anything involving an 'inverse angle'.:doh:
 
  • #29
OmCheeto said:
Has anyone determined what this means, mathematically?

By visible, does that limit us to human eyes and brain power?: 180° field of view, & resolution.
If not, then mathematically, we should be able to determine that the earth is curved from anything above zero altitude. A somewhat trivial problem which I solved several years ago.

If we are limited to human eyes and brains, then google claims we have to be at an altitude of 35000 feet to 'visually' see it.

Joining a little late but it seems to me the OP is talking about how an observer would see a segment of the horizon in a limited view - as if projected on a plane perpendicular to his line-of-sight. It would still be a circle but, being a different field-of view, it seems the apparent size would be different. (But I may be talking out of my hat. Dammit Jim! I'm a photographer, not a geometer).

Wide-angle shots versus human-eye-esque fields-of-view tend to greatly distort the proportions of objects.
1738553480073.png



OmCheeto said:
In any event, I'm confused how to measure 'visible curvature' in other than in binary terms: 'Yes' it's curved, and 'No' it's not.
It would be quantifed as a subtended angle of the observer's view, just like any other object.
"At altitude X the horizon appears as a segment of a circle whose radius/diameter subtends Y degrees in my field of view."

Because of the limited field of view, and the oblique angle of observation I am not sure that the circle in diagram B (above) would appear to the observer to be the same radius as it would in diagram A.
 
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  • #30
DaveC426913 said:
Joining a little late but it seems to me the OP is talking about how an observer would see a segment of the horizon in a limited view - as if projected on a plane perpendicular to his line-of-sight.
Yes, exactly, thank you. However, the horizon circle would not be at the angle shown in your diagram, but rather at the angle that I've added in yellow. When the observer is looking at the central point of the horizon (from his point of view), he will be viewing the horizon circle at an inclined angle, so the circular arc of the horizon will be seen as an elliptical arc, due to foreshortening of the horizon circle arc in the direction in which the observer is looking.
 

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  • #31
DaveC426913 said:
Joining a little late but it seems to me the OP is talking about how an observer would see a segment of the horizon in a limited view - as if projected on a plane perpendicular to his line-of-sight. It would still be a circle but, being a different field-of view, it seems the apparent size would be different. (But I may be talking out of my hat. Dammit Jim! I'm a photographer, not a geometer).

Wide-angle shots versus human-eye-esque fields-of-view tend to greatly distort the proportions of objects.
View attachment 356738
In the upper diagram, which you've marked with an X, the red line represents the horizon. In the second diagram the red line does not represent the horizon. The red line below the apex would be hidden behind the horizon. The horizon must be symmetrical in all directions. If it's an ellipse, then what defines the major and minor axes?
 
  • #32
ScarBest said:
When the observer is looking at the central point of the horizon (from his point of view), he will be viewing the horizon circle at an inclined angle, so the circular arc of the horizon will be seen as an elliptical arc, due to foreshortening of the horizon circle arc in the direction in which the observer is looking.
I do not believe that. The observer is at the apex of a cone, the horizon is tangent with the sphere. The distance to the horizon, from the observer, is the same in any direction. The horizon will always be part of a circle, never an ellipse. To get an ellipse, you must cut a diagonal plane through a cone, but the horizon is a cut perpendicular to the axis, so must remain a circle, when viewed from the apex.
 
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  • #33
PeroK said:
In the upper diagram, which you've marked with an X, the red line represents the horizon. In the second diagram the red line does not represent the horizon.
Diagram not-to-scale.

PeroK said:
The red line below the apex would be hidden behind the horizon. The horizon must be symmetrical in all directions. If it's an ellipse, then what defines the major and minor axes?
The point I am trying to draw attention to is the axis of the observer's line of sight. (The centre, dotted red arrow), and the observed angle of the arc of the horizon is perpendicular to that.

A camera would show this by projecting the curve onto its focal plane, which is perpendicular. Closing one eye would also achieve the same effect - by removing any clues about distance and foreshortening. @ScarBest: This is why I think your yellow line annotation is incorrect. But I may be misinterpreting you.


In diagram A, the observer's line of sight coincides with the centre of the circle - the horizon equidistant in all directions. And the viewing angle of the horizon is highly acute (magenta) not perpendicular.

In diagram B, it lines up with the horizon's near edge, and is perpendicular to it (magenta). Only a portion of the horizon is visible, most of it being off the bottom of the observer's field-of-view.




1738594089789.png
 
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  • #34
DaveC426913 said:
Diagram not-to-scale.


The point I am trying to draw attention to is the axis of the observer's line of sight. (The centre, dotted red arrow), and the observed angle of the arc of the horizon is perpendicular to that.

A camera would show this by projecting the curve onto its focal plane, which is perpendicular. Closing one eye would also achieve the same effect - by removing any clues about distance and foreshortening. @ScarBest: This is why I think your yellow line annotation is incorrect. But I may be misinterpreting you.


In diagram A, the observer's line of sight coincides with the centre of the circle - the horizon equidistant in all directions. And the viewing angle of the horizon is highly acute (magenta) not perpendicular.

In diagram B, it lines up with the horizon's near edge, and is perpendicular to it (magenta). Only a portion of the horizon is visible, most of it being off the bottom of the observer's field-of-view.




View attachment 356757
Unless you get into the optics of an eye or camera lens, the horizon is a horizontal cut of a cone and is hence a circle. Even projected to an intermediate horizontal plane, you get a circle.

The right angle in the second diagram makes no sense to me in terms of points on the horizon.
 
  • #35
PeroK said:
Unless you get into the optics of an eye or camera lens,
Exactly so. The OP mentions at least once or post that he is talking about what the observer sees visually.

If the observer looked out the window of his craft, with the horizon vertically centred, and the window perpendicular to his line-of-sight, he could draw an arc right on the window with a sharpie.

This arc would be of a portion circle/ellipse that would subtend a measurable amount of his view (at that specific distance from the window).

1738602383560.png


I doubt the radius of that curve would be the same as the actual horizon if he were looking straight down on the Earth, because, looking out the porthole like this, the rest of the horizon wouldn't be below his feet, it would be literally behind him, almost viewable out the opposite porthole.

PeroK said:
The right angle in the second diagram makes no sense to me in terms of points on the horizon.
It's no longer points on a horizon; It's a curve on a plane perpendicular to the observer. That curve is what the observer sees, absent any 3-dimensional/foreshortening clues.

Maybe I've got it wrong. If the OP can't seem to nail down a description of what he's doing, I'm not going to do much better.
 
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