Do the classics still work? and horizons

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Discussion Overview

The discussion revolves around the applicability of classical projectile motion equations in the context of large distances and the curvature of the Earth. Participants explore how these equations might be adjusted or interpreted when considering the Earth's surface and the concept of the horizon, including calculations related to visibility from different heights.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Mathematical reasoning

Main Points Raised

  • One participant questions whether the projectile equations remain valid when initial velocities are high enough for projectiles to travel beyond the horizon, and how these equations account for the Earth's curvature.
  • Another participant argues that Cartesian coordinates may not be appropriate when considering the Earth's curvature, suggesting that polar coordinates could be a better model for projectile motion.
  • It is noted that the projectile's path would not be strictly parabolic at very large distances due to the changing direction of acceleration, with an example given of an orbiting asteroid following a circular path.
  • A participant provides a mathematical approach to calculating the distance to the horizon based on an observer's height, referencing the relationship between height and the Earth's diameter.

Areas of Agreement / Disagreement

Participants express differing views on the validity of classical projectile motion equations in the context of Earth's curvature, with some proposing alternative coordinate systems. The discussion remains unresolved regarding the best approach to model projectile motion over large distances.

Contextual Notes

There are assumptions regarding the applicability of classical mechanics in non-ideal conditions, such as the curvature of the Earth and the height of the observer. The mathematical derivations presented depend on specific conditions and approximations that may not hold universally.

Who May Find This Useful

This discussion may be of interest to students and enthusiasts of physics, particularly those exploring classical mechanics, projectile motion, and the effects of Earth's curvature on motion. It may also appeal to those interested in mathematical modeling and calculations related to visibility and distance on spherical surfaces.

Phymath
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in a case were we use a lot of inital velocity, does the projectiles equations
([tex]x = x_0 + v_0t + \frac{1}{2}at^2[/tex]) still hold I mean when its range is so large that it actually will go beyond the horizon? How does the equation compensate for a rounded surface or does it not have to? btw how far is the horizon for an average humans height, how do u figure that out for a given height?
 
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I would say cartesian coordinates are not valid when the curvature of the Earth is taken into account into the projectile equations. Surely [tex]\overline{g}[/tex] will not point towards the "-y" direction but "-r" direction, and both x and y coordinates will have a component of [tex]\overline{g}[/tex]

Anyway, you can model such projectile with polar coordinates, no matter what initial velocity has. In the limit in which the radius of curvature of the ground tends to zero (small trajectories), the polar coordinates collapses over cartesian coordinates.
 
The projectile would not follow a strictly parabolic curve if you go *very* far out since the acceleration would not be in the same direction. An extreme example would be an orbiting asteroid, but in this case it would follow a circle-ish shape. I think those problems would be a lot easier to solve using work and energy, just a thought.
 
Phymath said:
btw how far is the horizon for an average humans height, how do u figure that out for a given height?

Phymath that is a nice question and IIRC the answer is like this.

To a good approx, on a sphere, when you are height h above surface,
the distance X from your eye to horizon is the solution to this:

X/h = D/X, where D is diameter of sphere

So let us say diameter of Earth is 8000 miles and you are 125 miles above surface, so

X/125 = 8000/X

then to solve
X2 = 1000 000
X = 1000 miles

that is, if you are 125 miles high then you can see 1000 miles

or, if you are 1.25 miles high, then you can see 100 miles.

Another way to write formula is

X2 = Dh = 2Rh
where h is height of observer and R is radius of sphere.

the proof is by pythagoras triangle formula and simple picture
and an approx which depends on h being small compared with R.
 
thanks man!
 

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