Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the...

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Chapter: Earth’s Place in Space Table of Contents Section 3: Earth and the Solar System Section 1: Earth’s Motion and Seasons Section 2: Earth’s Moon

Transcript of Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the...

Page 1: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

Chapter: Earth’s Place in Space

Table of ContentsTable of Contents

Section 3: Earth and the Solar System

Section 1: Earth’s Motion and Seasons

Section 2: Earth’s Moon

Page 2: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• In the past, some people thought that the Sun, the Moon, and other objects in space moved around Earth each day.

• Now it is known that some of the motions of these objects, as observed from Earth, are really caused by Earth’s movements.

Earth’s Physical Data11Earth’s Motion and SeasonsEarth’s Motion and Seasons

Page 3: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Pictures from space show that Earth is shaped like a ball, or a sphere.

Spherical Earth11

• A sphere (SFIHR) is a three-dimensional objectwhose surface at all points is the same distance from its center.

Earth’s Motion and SeasonsEarth’s Motion and Seasons

Page 4: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• More proof of Earth’s shape is that Earth casts a curved shadow on the Moon during a lunar eclipse.

• Something flat, like a book, casts a straight shadow, whereas objects with curved surfaces cast curved shadows.

Evidence for Earth’s Shape11Earth’s Motion and SeasonsEarth’s Motion and Seasons

Page 5: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Gravity is a force that attracts all objects toward each other.

• Large objects in space, such as planets and moons often are spherical because of how they formed.

Influence of Gravity11

• At first, particles collide and stick together randomly. However, as the mass increases, gravity plays a role.

• Particles are attracted to the center of the growing mass, making it spherical.

Earth’s Motion and SeasonsEarth’s Motion and Seasons

Page 6: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Earth’s shape is not a perfect sphere. It bulges slightly at the equator and is somewhat flattened around the poles.

Almost a Sphere11Earth’s Motion and SeasonsEarth’s Motion and Seasons

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Almost a Sphere11

• This causes Earth’s circumference at the equator to be a bit larger than Earth’s circumference as measured through the north and south poles.

• The circumference ofEarth and some otherphysical properties are listed in this table.

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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Almost a Sphere

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Page 9: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Earth’s geographic poles are located at the north and south ends of Earth’s axis.

Motions of Earth

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Motions of Earth

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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• Earth’s axis is the imaginary line drawn from the north geographic pole through Earth to the south geographic pole.

Page 11: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• The spinning of Earth on its axis, called rotation, causes you to experience day and night.

Motions of Earth

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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Earth’s Orbit

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• As it rotates on its axis each day, Earth also moves along a path around the Sun. This motion of Earth around the Sun is calledrevolution.

Page 13: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

Earth’s Orbit

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• What happens on Earth that is caused by its revolution?

Page 14: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Earth is really a satellite of the Sun, moving around it along a curved path called an orbit.

Seasons

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• As Earth moves along in its orbit, the way in which the Sun’s light strikes Earth’s surface changes.

Page 15: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Earth’s elliptical orbit causes it to be closer to the Sun in January and farther from the Sun in July.

Seasons

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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• The amount of energy that specific places on Earth receive varies quite a lot.

Page 16: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Earth’s axis forms a 23.5-degree angle with a line perpendicular to the plane of its orbit around the Sun.

Earth’s Tilt

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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• Because of this, there are more daylight hours for the hemisphere tilted toward the Sun.

Page 17: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Sunlight strikes the hemisphere tilted toward the Sun at a higher angle, that is, closer to 90 degrees.

Earth’s Tilt

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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Earth’s Tilt

Earth’s Motion and SeasonsEarth’s Motion and Seasons

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• Sunlight strikes the hemisphere tilted away from the Sun at a lower angle. This lessens solar radiation and brings winter.

Page 19: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Twice during the year, the Sun reaches its greatest distance north or south of the equator and is directly over either the Tropic of Cancer or the Tropic of Capricorn.

Solstices

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• These times are known as the summer and winter solstices.

Page 20: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• Summer solstice is when the Sun is highest in the sky at noon.

Solstices

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• The opposite of this for each hemisphere is winter solstice, which is when the Sun is lowest at noon.

Page 21: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

• At an equinox, (EE kwuh nahks) when the Sun is directly above Earth’s equator, the lengths of day and night are nearly equal all over the world.

Equinoxes

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• During equinox, Earth’s tilt is neither toward nor away from the Sun.

Page 22: Chapter: Earths Place in Space Table of Contents Section 3: Earth and the Solar SystemEarth and the Solar System Section 1: Earths Motion and Seasons.

Section CheckSection Check

11Question 1

What evidence suggests that Earth is round?

AnswerObjects with curved surfaces cast curved shadows and Earth casts a curved shadow on the Moon during a lunar eclipse. Pictures from space show Earth as a ball or a sphere.

FL: SC.E.1.3.2

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11Section CheckSection Check

Question 2

Which is responsible for the change in seasons?

A. Earth’s orbitB. Earth’s revolutionC. Earth’s rotationD. summer solstice

FL: SC.E.1.3.1

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Answer

The answer is B. A revolution is completed when Earth completes one complete trip around the Sun. It takes one year for Earth to travel around the Sun.

FL: SC.E.1.3.1

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Question 3

What is it called when the length of day and night are equal all over the world?

A. equinoxB. lunar eclipseC. revolutionD. solstice

FL: SC.E.1.3.1

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Answer

The answer is A. An equinox occurs when the Sun is directly above Earth’s equator. During an equinox, Earth’s tilt is neither toward nor away from the Sun and the length of day and night all over the world is nearly equal.

FL: SC.E.1.3.1