Earth & Space Science

Earth & Space Science

  • About This Project
    • Preface/About
    • Author/Contributors
    • For Investors/Donors
    • Teaching Guide
  • Ch 1 – Our Place in the Universe
    • Chapter Introduction
    • 1.1 Our Cosmic Address
    • 1.1.1 Overview
    • 1.1.2 What do we mean when we say “Earth is a planet”?
    • 1.1.3 What is our solar system?
    • 1.1.4 What is a galaxy?
    • 1.1.5 What is the universe?
    • 1.1 Review: Our Cosmic Address
    • 1.2 The Scale of Space
    • 1.2.1 Overview
    • 1.2.2 How Big is the Earth–Moon System?
    • 1.2.3 How Big is our Solar System?
    • 1.2.4 How far are the stars?
    • 1.2.5 How big is the Milky Way Galaxy?
    • 1.2.6 How big is the universe?
    • 1.2 Review: The Scale of the Universe
    • 1.3 Spaceship Earth
    • 1.3.1 How is Earth moving in our solar system?
    • 1.3.2 How is our solar system moving in the Milky Way Galaxy?
    • 1.3.3 How does our galaxy move relative to other galaxies in the universe?
    • 1.3 Review
  • Ch 2 – Understanding the Sky
    • Chapter Introduction
    • 2.1 Our Everyday View of the Universe
    • 2.1.1 What do we see in the local sky?
    • 2.1.2 What is the celestial sphere?
    • 2.1.3 Why do stars rise and set?
    • 2.1.4 Why do we see different constellations at different times of year?
    • 2.1 Review
    • 2.2 Seasons
    • 2.2.1 What causes the seasons?
    • 2.2.2 How do seasons differ around the world?
    • 2.2.3 Does the orientation of Earth’s axis ever change?
    • 2.2 Review
    • 2.3 Viewing the Moon: Phases and Eclipses
    • 2.3.1 Why do we see phases of the Moon?
    • 2.3.2 When do we see different phases of the Moon in our sky?
    • 2.3.3 Why do we always see the same face of the Moon?
    • 2.3.4 What are eclipses?
    • 2.3 Review
    • 2.4 Planets in the Night Sky
    • 2.4.1 How do we recognize planets in the sky?
    • 2.4.2 Why do the planets “wander”?
    • 2.4 Review
  • Ch 3 – How Science Discovered the Earth
    • Chapter Introduction
    • 3.1 The Ancient View of Earth
    • 3.1.1 How did the ancient Greeks learn that Earth is round?
    • 3.1.2 Why didn’t the ancient Greeks realize that Earth orbits the Sun?
    • 3.1 Review
    • 3.2 The Copernican Revolution
    • 3.2.1 How did the idea of Earth as a planet gain favor?
    • 3.2.2 How did Galileo seal the case for Earth as a planet?
    • 3.2 Review
    • 3.3 The Nature of Modern Science
    • 3.3.1 How does science work?
    • 3.3.2 What is a “theory” in science?
    • 3.3.3 What is the value of science?
    • 3.3 Review
    • 3.4 The Fact and Theory of Gravity
    • 3.4.1 What is gravity?
    • 3.4.2 How does gravity hold us to the ground and make objects fall?
    • 3.4.3 Why does gravity make planets round?
    • 3.4.4 How does gravity govern motion in the universe?
    • 3.4 Review
  • Chapter 4 – Planet Earth
    • Chapter Introduction
    • 4.1 A Planetary Overview
    • 4.1.1 What does Earth look like on the outside?
    • 4.1.2 What does Earth look like on the inside?
    • 4.1.3 How has Earth changed through time?
    • 4.1.4 How do we study the Earth?
    • 4.1 Review
    • 4.2 Earth System Science
    • 4.2.1 What are Earth’s four major systems?
    • 4.2.2 What drives Earth system changes?
    • 4.2.3 What IS energy and how do we measure it?
    • 4.2 Review
    • 4.3 Earth In the Context of Other Worlds
    • 4.3.1 How does Earth compare to other worlds of our solar system?
    • 4.3.2 Could there be life on other worlds?
  • Chapter 5 – Earth Through Time
    • Chapter Introduction
    • 5.1 Learning from Rocks and Fossils
    • 5.1.1 How do rocks form?
    • 5.1.2 What are fossils?
    • 5.1.3 How do we learn the ages of rocks and fossils?
    • 5.1 Review
    • 5.2 Shaping Earth’s Surface
    • 5.2.1 How do continents differ from oceans?
    • 5.2.2 What processes shape continents?
    • 5.2.3 What dangers do geological changes pose?
    • 5.2 Review
    • 5.3 Plate Tectonics — The Unifying Theory of Earth’s Geology
    • 5.3.1 What evidence led to the idea that continents move?
    • 5.3.2 How does the theory of plate tectonics explain Earth’s major features?
    • 5.3 Review
    • 5.4 A Brief Geological History of Earth
    • 5.4.1 What major changes mark Earth’s fossil record?
    • 5.4.2 What killed the dinosaurs?
    • 5.4.3 Have we humans started a new geological epoch?
    • 5.4 Review
  • Chapter 6 – Air and Water
    • Chapter Introduction
    • 6.1 Atmosphere and Hydrosphere
    • 6.1.1 What exactly is the atmosphere?
    • 6.1.2 How is water distributed on Earth?
    • 6.1.3 How does water cycle through the hydrosphere and atmosphere?
    • 6.1 Review
    • 6.2 Global Winds and Currents
    • 6.2.1 What drives global winds and currents?
    • 6.2.2 What is the general pattern of winds on Earth?
    • 6.2.3 What is the general pattern of ocean currents?
    • 6.2 Review
    • 6.3 Weather and Climate
    • 6.3.1 What is the difference between weather and climate?
    • 6.3.2 How and why does climate vary around the world?
    • 6.3.3 How do we measure and predict the weather?
  • Chapter 7 – Human Impact on the Climate
    • Chapter Introduction
    • 7.1 The Basic Science of Global Warming
    • 7.1.1 What is the greenhouse effect?
    • 7.1.2 How is human activity strengthening Earth’s greenhouse effect?
    • 7.1.3 How do we know that global warming is really happening and is human-caused?
    • 7.1.4 How does human-caused climate change compare to natural climate change?
    • 7.1 Review
    • 7.2 Consequences of Global Warming
    • 7.2.1 What are the major consequences of global warming?
    • 7.2.2 How do scientists predict future consequences of global warming?
    • 7.2.3 How will climate changes affect you and others around the world?
    • 7.2 Review
    • 7.3 Solutions to Global Warming
    • 7.3.1 What existing technologies could solve the problem of global warming?
    • 7.3.2 What future technologies might help even more?
    • 7.3.3 What does it take to implement a solution?
    • 7.3.4 What will your world look like AFTER we solve global warming?
    • 7.3 Review

Do the Math

Eccentricity

We know planets move in ellipses, but what exactly is an ellipse?

Ellipses are squashed circles, and a property called eccentricity tells us just how squashed the circle is. Mathematically, eccentricity is defined as the ratio of the distance of each focus from the center of the ellipse, c, to the length of the semi-major axis, a :

Figure 1.

Physically this means that the shape of ellipses varies depending on the eccentricity. Figure 2 shows how ellipses can have an eccentricity of 0 to 0.9, where 0.9 represents the “most squashed” or elongated. Notice how an eccentricity of 0 represents an ellipse with no elongation, or a circle. In other words, a circle is a special case of an ellipse with 0 eccentricity.

Figure 2.

Knowing the eccentricity of an orbit allows us to learn some other interesting physical characteristics about any orbiting body. Perihelion is defined as the point in an orbit where the planet is closest to the sun. Aphelion (pronounced “app-helion”) is the point in its orbit where a planet is farthest from the sun, as shown in Figure 3. Since eccentricity defines the shape of an ellipse about its foci, we can use e to calculate the perihelion and aphelion distances of a planet, using the formulae below:

 
 
 
 

Perihelion distance = a (1-e)

Aphelion distance = a (1+e)

Figure 3.

Using the information we just learned, let us answer the questions: At its closest, how far away is Mercury from the Sun? How far away is it at the farthest point in its orbit?

Step 1: Understand the problem

The question is asking you “how far”, which means you are looking for a distance. Specifically, the first question is asking for the shortest distance between Mercury and the Sun. In the discussion above, you learned that this distance is called the perihelion distance, and it can be calculated using the formula:

Perihelion distance = a (1-e)

Similarly, the second question is also asking for a distance (“how far away . . .”), specifically the largest distance between Mercury and the Sun. You know this distance is defined as the aphelion distance, and you can calculate it using the formula:

Aphelion distance = a (1+e)

Step 2: Solve

To solve this problem you will need a few values. The eccentricities and semi-major axes of the planets have all been carefully measured and verified, are shown in Table 1. You can use these values to solve your equations for perihelion and aphelion distances.

 
 
 
 

Table 1

Step 3: Explain

From this calculation we can see that the eccentricity in its orbit means Mercury’s distance from the Sun varies by almost 24 million km, depending on where it is in its orbit. In fact, as you can see from Table 1, Mercury has the most eccentric orbit of all the eight planets in our solar system.

Check your Skills:

Following the example for Mercury, calculate the perihelion and aphelion distances for the Earth.

Check your skills
Following the example for Mercury, calculate the perihelion and aphelion distances for the dwarf planet Eris.

Show Teachers Notes

This section teaches students about the eccentricity of planet orbits and how this property can help us learn about the physical characteristics of a planet’s orbit. The example walks students through the calculations to determine how close a planet will get to the sun during its orbit (the perihelion distance), as well as the calculation for determining the farthest distance a planet will reach (aphelion distance) away from the Sun.

In the check your skills sections, students can compare the difference in distances between Earth and the dwarf planet Eris. They should notice that Earth, with its low eccentricity of 0.017 varies by only a few million km (~5 million km), which is less than 4 percent of its average orbital distance (also called semi-major axis) from the Sun. Eris provides a stark contrast, with the highest eccentricity of objects in the solar system (e = 0.4412). Eris’s distance from the sun varies by 8,971 million km, depending on where it is in its orbit. This is 88 percent (!) of its average orbital distance or semi-major axis. Students can verify this for themselves by looking up diagrams of the orbits of objects in the solar system, and they will see how Eris’s orbit looks much more elongated than any of the planets, whose orbits look nearly circular due to their relatively low eccentricities.

The answers to the check your skills boxes are shown below:

Check your skills (Earth):
Perihelion distance = (149.6×106 km) x (1-0.017)

= 147.1×106 km

Aphelion distance = (149.6×106 km) x (1+0.017)

= 152.1×106 km

Check your skills (Eris):
Perihelion distance = (10,166×106 km) x (1-0.4412)

= 5,680×106 km

Aphelion distance = (10,166×106 km) x (1+0.4412)

= 14,651×106 km

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