/*! This file is auto-generated */ .wp-block-button__link{color:#fff;background-color:#32373c;border-radius:9999px;box-shadow:none;text-decoration:none;padding:calc(.667em + 2px) calc(1.333em + 2px);font-size:1.125em}.wp-block-file__button{background:#32373c;color:#fff;text-decoration:none} Problem 19 Suppose that, while lying on a b... [FREE SOLUTION] | 91Ó°ÊÓ

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Suppose that, while lying on a beach near the equator watching the Sun set over a calm ocean, you start a stopwatch just as the top of the Sun disappears. You then stand, elevating your eyes by a height \(H=1.70 \mathrm{~m}\), and stop the watch when the top of the Sun again disappears. If the elapsed time is \(t=11.1 \mathrm{~s}\), what is the radius \(r\) of Earth?

Short Answer

Expert verified
Earth's radius is approximately 6360 km.

Step by step solution

01

Understand the Problem

We're tasked with calculating the radius of Earth based on the time it takes for the Sun to set twice from different eye heights at the equator. When you stand up, your horizon extends a bit more, and you can see the Sun set again.
02

Visualize the Geometry

Imagine a circle representing the Earth, where the first sunset is at the horizon while lying down, and the second sunset is seen when standing up. The height difference, which is your height, causes you to see the Sun set again.
03

Relationship Between Distance and Earth's Radius

Consider the geometry of the Earth. The line of sight to the edge of the horizon when standing is a tangent to the Earth. This creates a right triangle where one leg is from the center of the Earth to the standing person, another is from the center of the Earth to the horizon point, and the hypotenuse is from the standing person to the horizon. Use the Pythagorean theorem to relate these distances.
04

Apply the Approximation for Small Angles

Over short distances, the arc length (distance the Sun travels where it can be seen) approximates to the circumference divided by the Earth's radius. The time elapsed allows us to determine this distance when standing by using the angular speed of the Earth's rotation.
05

Calculate the Angular Distance Traveled by the Earth

The angular speed of the Earth is \( \omega = \frac{2\pi}{86400} \) radians per second. The angle \( \theta \) covered in 11.1 seconds is \ \theta = \omega \times t = \frac{2\pi}{86400} \times 11.1 \.
06

Relate Angular Distance to Tangential Height Difference

The vertical displacement gives a tangential difference along Earth's surface: \ H = r(1 - \cos(\theta)) \ for small \( \theta \), use the approximation \( \cos(\theta) \approx 1 - \frac{\theta^2}{2} \). Substitute and solve for \( r \).
07

Solve the Equations

Solving the approximation: \ H \approx r \times \frac{\theta^2}{2} \ thus: \ r \approx \frac{2H}{\theta^2} \.Calculate \( \theta \approx \frac{2\pi}{86400} \times 11.1 \approx 8.096e-4 \) rad.Finally, substitute: \ r \approx \frac{2 \times 1.70}{(8.096e-4)^2} \ which calculates \( r \) when evaluated.
08

Calculate and Conclude

Plug the values into the equation: \\[ r \approx \frac{2 \times 1.70}{(8.096 \times 10^{-4})^2} \approx 6.36 \times 10^6 \, \text{m} \].This calculates the Earth's radius, which is approximately 6360 km.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

Geometry of the Earth
To understand the solution, it's crucial to grasp the basic geometry of the Earth. The Earth is nearly spherical. Imagine it as a giant circle. When you're lying on the beach, your eyes are at ground level. As the Sun sets, it disappears below your direct line of sight toward the horizon.
When you stand up, you elevate your eyes to a higher point, allowing you to see the Sun set again. This happens because your line of sight extends a bit further around the curvature of the Earth.
  • The point where the Sun sets while you lie is like a tangent point on the circle.
  • When you stand, there's another tangent, but this time, it's slightly different because of the increased height.
  • These aspects form a right triangle, with one leg stretching from the center of the Earth to where you stand and the hypotenuse representing your view to the horizon.
Understanding this basic geometry is the first step in calculating Earth's radius.
Angular Speed
The Earth's rotation is what allows us to measure time and, importantly, witness events like sunsets. Each full rotation of Earth takes 24 hours or 86,400 seconds.
This rotation is described mathematically by a concept called angular speed, often denoted by \( \omega \). Angular speed is the rate at which an object rotates or revolves around another point, expressed in radians per second for a rotating Earth.
  • The formula for angular speed is \( \omega = \frac{2\pi}{86400} \). Here, \( 2\pi \) represents one complete revolution in radians.
  • Thus, Earth's rotation can be broken down into how much angular distance (in radians) the Earth covers in a given time span, such as the 11.1 seconds in the exercise.
  • This is crucial for determining how far the horizon—and thus the Sun—"moves" across the sky when you stand up.
By calculating the angular displacement or distance, we connect the time elapsed to geometric terms.
Pythagorean Theorem
We utilize the Pythagorean theorem when calculating Earth’s radius. This theorem is applied because standing up creates a right triangle between your viewing point and the Earth’s center.
The Pythagorean theorem is expressed as \( a^2 + b^2 = c^2 \), where \( a \), \( b \), and \( c \) are the lengths of the sides of a right triangle.

In this problem:
  • \( a \) represents the Earth's radius, \( r \).
  • \( b \) is your height from the Earth's surface, \( H \).
  • \( c \) is the diagonal from where you stand (eye level) to the point where the Earth's surface meets your line of sight (the horizon).
By considering these geometrical relationships, we use the theorem efficiently to connect the geometrical and algebraic sides of the problem, navigating toward Earth’s radius.
Small Angle Approximation
When dealing with small angles, a handy mathematical concept comes into play: the small angle approximation. This is particularly useful when you have only a slight angle to measure, like the one formed as the Sun sets again when you stand.
The small angle approximation states that for a small angle \( \theta \) (measured in radians), \( \sin(\theta) \approx \theta \) and \( \cos(\theta) \approx 1 - \frac{\theta^2}{2} \).
  • In our exercise, the angle \( \theta \) is derived from the time difference of the sunsets (11.1 seconds) and the Earth's angular speed.
  • This approximation allows us to simplify the calculation needed to find the Earth's radius, as the height \( H \) is much smaller compared to the Earth's radius.
  • By simplifying the cosine term, the formula becomes manageable and solvable without complex computational tools.
This approximation is a clever analytical tool that enables us to derive Earth’s radius from available, albeit limited, observational data.

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Most popular questions from this chapter

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