# Derivation of the Formula Eight Inches per Miles squared

Monday, April 16, 2018 - 17:52 | Author: wabis | Topics: FlatEarth, Mathematic, Geometry
There is a famous formula that Flat Earthers frequently use to calculate the curvature of the Globe Earth. This formula is an approximation. Here I derive the exact formulas and the approximation 8" per miles squared and compare the results in a Calcularor Form.

## Drop-Formula

Sketch 1
(1)
 x = 8" \cdot s^2
where'
 x ' =' 'drop from the plane which is tangential to the surface at the observer, in inches (1" = 1 in = 0.0254 m) s ' =' 'distance from observer along the surface in statute miles (1 mi = 1609.344 m)

This formula is an approximation with an error of less than 0.1% if s is smaller than 799.9 km or 497.0 mi.

Note that this function underestimates the correct value at distances less than 391.1 km or 243.1 mi, so at this distance it is the most accurate. At 1 mi or 1.609 km its error is about 0.0314% and decreases until 391.1 km or 243.1 mi. On longer distances the error starts to increase again. At 799.9 km or 497.0 mi the error is about 0.1%. At 2234 km or 1388 mi the error is about 1% and then rapidly increasing.

The deviation of the approximated value from the real value is shown in the Calculator Form at ~x - x absolute or as the relative error in % in the orange field (~x-x)/x.

This approximation formula can also be used to approximate h, since for distances less than 258.5 km or 160.2 mi the error for h is less than 0.1%. But generally h is always greater than x and the deviation between them grows exponentially.

## Calculator Form

Sketch 1 shows the values used in the calculator form. Variables preceded with a ~ are calculated using the approximation formulas, all other variables are calculated using the correct formulas.

## Curvature, Hidden Parts and Refreaction

Strictly speaking x is not the curvature of the earth but the drop from the tangential plane (blue line in Sketch 1) at a distance s from the observer. The curvature k of a sphere is defined as the reciprocal of its radius: k = 1 / r.

The drop x is not what is hidden by the curvature of the earth! This would only be the case if the observers eyes are at the surface. If the observers eyes are at an altitude greater than 0 the hidden part is less than x. In fact if the observer is high enough it can always see the whole object in the distance.

Standard Refraction bends light downwards in an arc with a radius of about 7 times the radius of the earth. This means that far objects get lifted and can come into view from behind the horizon. On warm air over cold water or ice refraction can be considerably greater, so that the arc radius of the light can get smaller than the radius of the earth. In this case the earth looks flat or even concave and you can see shores in great distances, what explains many of the flat earthers LASER test done over a frozen or cold lake.

## How the Drop-Formula is derived

I will derive the exact formulas for h and then x from s and r and then show how the approximation for x is derived from that and why it is accurate enough as long as s is much smaller than r.

Sketch 1

First we need the angle a, that can be calculated from s and r. On a circle with radius r = 1 the circumference is 2π, which is also the angle a of the full circle. So the angle a in radian of a unit circle is always equal to the length of a corresponding segment of length s. If we have a circle of radius r instead, we simply have to divide s through r to get the corresponding angle a:

(2)
 a = s / r
where'
 a ' =' 'angle in radian s ' =' 'circle segment length r ' =' 'radius of the circle

The distance d can now be calculated from the angle a and the radius r. The tangent of the right-angled triangle [r,d,r+h] is tan(a) = d / r. Solving for d gives:

(3)
 d = r \cdot \tan( a ) = r \cdot \tan( s/r )

Using Pythagoras we can now calculate h:

 (4) d^2 + r^2 = (r + h)^2

We expand the square on the right hand side:

 (5) d^2 + \color{red}{r^2} = \color{red}{r^2} + 2 \cdot r \cdot h + h^2

The radius squared can be subtracted from both sides:

 (6) d^2 = 2 \cdot r \cdot h + h^2

We can rearrange this formual to get a quadratic equation for the unknown h:

 (7) h^2 + 2 \cdot r \cdot h - d^2 = 0

Inserting d from (3) gives the following quadratic equation for h:

(8)
 h^2 + 2 \cdot r \cdot h - \left[ \ r \cdot \tan( s/r ) \ \right]^2 = 0

To calculate h we can use the method for solving a Quadratic equation. We substitute p = 2·r and q = −[r·tan(s/r)]2 to get the normal form of the quadratic equation:

 (9) h^2 + p \cdot h + q = 0

Solving the quadratic equation for h gives the two solutions:

 (10) h = - { p \over 2 } \pm \sqrt{ \left( { p \over 2 } \right)^2 - q }

We are only interested in the positive solution:

 (11) h = \sqrt{ \left( { p \over 2 } \right)^2 - q } - { p \over 2 }

In our case is p = 2·r and q = −[r·tan(s/r)]2:

Sketch 2
 (12) h = \sqrt{ r^2 + r^2 \cdot \tan^2(s/r) } - r

Factoring out r we finally get a formula for h:

(13)
 h = r \cdot \left( \sqrt{ 1 + \tan^2(s/r) } - 1 \right)

Here is another equivalent formula for h:

(14)
 h = r \cdot { 1 - \cos(s/r) \over \cos(s/r) }

We can see in Sketch 2 that, using trigonometry, x = rr·cos(a). Factoring out r gives:

(15)
 x = r \cdot \left[ 1 - \cos( s/r ) \right]

Note that

 (16) h = { x \over \cos(a) }

which can be seen from Sketch 1. This is how (14) is derived.

## Approximation Formula for x

We can simplify the derived formulas (15), (13) and (14) by taking advantage of the fact that in practice s is much smaller than r. In this case the angle a is very small and we can replace the tan and cos functions by the first 2 terms of the corresponding Taylor series. We will see that in this approximations the length x and h will be the same.

Lets find first an approximation for x from the formula (15):

 (17) x = r \cdot \left[ 1 - \cos( s/r ) \right]

The cos function can be approximated by its taylor series:

 (18) \cos(a) = 1 - { a^2 \over 2! } + \color{red}{ { a^4 \over 4! } - { a^6 \over 6! } + ...}

Note ! is the factorial function: n! = 1·2·3·...·n, so 2! = 1·2 and 4! = 1·2·3·4 etc.

Now if a is much smaller than 1, then a4, a6... are even much, much smaller than 1. So these terms are negligible and we can simplify the cos function because the red terms do not contribute much to the result:

 (19) \cos(a) \approx 1 - { a^2 \over 2 } \text{if} \quad a = s/r \ll 1 \qquad \text{or} \qquad s \ll r

The symbol \ll means much less than. So s \ll r means s is much smaller than r.

Lets plug in this into (17):

 (20) x = r \cdot \left[ 1 - \color{blue}{\cos( s/r )} \right] \approx r \cdot \left[ 1 - \color{blue}{ \left( 1 - { (s/r)^2 \over 2 } \right) } \right] = r \cdot \left[ \color{red}{1 - 1} + { (s/r)^2 \over 2 } \right]

The red 1's cancel and we finally get:

(21)
 x \approx { s^2 \over 2\,r }
\text{if} \quad s \ll r

## The 8-inch per Miles squared Formula

We have now seen that for the case that s \ll r we get the same approximation for x:

(22)
 x \approx { s^2 \over 2\,r }

\text{if} \quad s \ll r

How do we get to 8" per miles squared? We are almost done. We only have to put in the radius of the earth r in miles so the result is in statute miles. Than we multiply by a conversion factor c = 63,360 in/mi to get inches from miles. The constants can be collected together and we get:

 (23) x \approx { c \over 2\, r } \cdot s^2 = { 63{,}360\ \mathrm{in}/\mathrm{mi} \over 2 \cdot 3958{.}8\ \mathrm{mi} } \cdot s^2 = 8{.}0024\ \mathrm{in}/\mathrm{mi}^{2} \cdot s^2

We round 8.0024 to 8 and finally get:

(24)
 x \approx 8\ \mathrm{in}/\mathrm{mi}^{2} \cdot s^2 = \text{ 8" per miles squared }
where'
 x ' =' 'drop from the plane, horizontal at P, in inches s ' =' 'distance along the surface in statute miles

## Approximation Formula 1 for h

Now lets find an approximation formula for h using the first formula (13):

 (25) h = r \cdot \left( \sqrt{ 1 + \tan^2(s/r) } - 1 \right)

The tan function taylor series is:

 (26) \tan(a) = { \sin(a) \over \cos(a) } = { a - \color{red}{(a^3 / 3!) + (a^5 / 5!) - ...} \over 1 - \color{red}{(a^2 / 2!) + (a^4 / 4!) - ...} }

Now if a is much smaller than 1, then a2, a3, a4 ... are even much, much smaller than 1. So these terms are negligible and we can simplify the tan function because the red terms do not contribute much to the result:

 (27) \tan(a) \approx a \text{if} \quad a = s/r \ll 1 \qquad \text{or} \qquad s \ll r

So if we plug in this into (25) we get:

 (28) h = r \cdot \left( \sqrt{ 1 + \color{blue}{\tan^2(s/r)} } - 1 \right) \approx r \cdot \left( \sqrt{ 1 + \color{blue}{(s/r)^2} } - 1 \right)

We can even simplify more, if we use the taylor series for 1 + x2:

 (29) \sqrt{ 1 + x^2 } \approx 1 + { x^2 \over 2 } \text{if} \quad x \ll 1

If we plug in this into (28) we get:

 (30) h \approx r \cdot \left( \color{blue}{ \sqrt{ 1 + (s/r)^2 } } - 1 \right) = r \cdot \left[ \color{blue}{ \left( \color{red}{1} + { (s/r)^2 \over 2 } \right) } \color{red}{- 1} \right]

The red 1 and −1 cancel and we finally get:

(31)
 h \approx x \approx { s^2 \over 2 \, r }
\text{if} \quad s \ll r

## Approximation Formula 2 for h

We can simplify the second formula (14) for h in a similar fashion as shown above.

 (32) h = r \cdot { 1 - \cos(s/r) \over \cos(s/r) }

The cos function taylor series is:

 (33) \cos(a) = 1 - (a^2 / 2!) + \color{red}{(a^4 / 4!) - (a^6 / 6!) + ...}

For small angles a we can omit the red terms, because they do not contribute to the result. If we plug in this into (32) we get:

 (34) h \approx r \cdot { 1 - \left( 1 - a^2/2 \right) \over 1 - a^2/2 } = r \cdot { a^2/2 \over \color{red}{1 - a^2/2} }

If a1 then a2/2 is even much smaller than 1, so we can replace the red term by 1:

 (35) h \approx r \cdot a^2 / 2 = { r \cdot (s/r)^2 \over 2 } = { r \cdot s^2 \over 2 \cdot r^2 }

And we get finally the same result as in the section above:

(36)
 h \approx x \approx { s^2 \over 2\,r }
\text{if} \quad s \ll r
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