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

I was wondering...

What about Satellites?

Although all “distant celestial objects” must rise in the east and set in the west, you may recall from Chapter 2 that it is possible for artificial satellites to do the opposite. But why? The answer lies with the time it takes satellites to orbit Earth.

Remember that it is Earth’s rotation, not any real motion of celestial objects, that explains why all “distant celestial objects” rise in the east and set in the west. This is true even for the Moon, because even though the Moon is orbiting Earth, it takes the Moon much longer than day (recall that it takes nearly a month) to complete one orbit.

The situation can be different for artificial satellites, which are human-made spacecraft that have been launched into orbit around Earth. Most satellites are launched into orbits that go around Earth in the same direction that Earth rotates. However, many of these go around faster than Earth rotates. For example, satellites in low-Earth orbit, such as the International Space Station, complete an orbit in only about 90 minutes, which means they are “outracing” Earth’s rotation.

Think now about what you see if you are in the passenger seat of a car and focus on another car as you approach and pass it on the freeway. Even though the other car is going in the same direction as you, your faster speed will make it appear to be moving backward relative to you.

In the same way, the fact that satellites in low-Earth orbit are going faster than Earth is rotating will make them appear to go backward (west to east) across our sky. You can often see this in the night sky, because many satellites in low-Earth orbit reflect enough sunlight to be visible to the naked eye when they are near the horizon. (They tend to disappear from view as they go higher overhead, because they are then in Earth’s shadow so that no sunlight reflects off of them.)

Interestingly, the planet Mars has a similar case with the larger of its two moons, Phobos. Phobos orbits Mars in less time than a Martian day. Therefore, even though all other celestial objects rise in the east and set in the west on Mars just as on Earth, Phobos does the opposite, traveling west to east across the Martian sky.

Note that not all artificial satellites are in low-Earth orbit (where we can see their reflected light) and not all orbit in the same direction that Earth rotates. Three other common cases are the following:


 
 
 

  • Medium altitude orbits: Some satellites, including those of the Global Positioning System (GPS), orbit at much higher altitudes than low-Earth orbit, but still low enough that they orbit faster than Earth rotates. These satellites are generally not visible because they are too far away.
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  • Geostationary orbit: This is an orbit above Earth’s equator at an altitude of about 36,000 kilometers, which is the altitude at which a satellite’s orbital period will match Earth’s rotation period. As a result, satellites in geostationary orbit always remain above the same point on Earth’s surface. Most communications satellites are in geostationary orbits, and this is why satellite dishes can remain pointed in the same direction (toward a particular satellite) at all times.
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  • Polar orbits: These are orbits that go around Earth’s north and south poles. As Earth rotates, a satellite with a polar orbit will pass over different portions of Earth (different longitude) with each orbit. Polar orbits are therefore particularly useful for satellites that seek to study the whole planet, because they are the only satellites that will repeatedly pass over every point on Earth.

The following animation shows how a satellite’s orbital speed and orbital period depends on its altitude. Be sure to notice that the satellites in low-Earth orbit are moving much faster than Earth is rotating. Also notice that the outermost circle shows a geostationary orbit that always remains above the same point on Earth’s surface. (Note: the “radius of orbit” shown in the animation is the distance from the center of the Earth, rather than the altitude above Earth’s surface.)

Diagram of different satellite orbits. Credit: Wikimedia Commons.

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