lecture 2: motions of the earth and...

63
Lecture 2: Motions of the Earth and Moon Astronomy 111

Upload: others

Post on 31-May-2020

1 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

Lecture 2: Motions of the Earth and Moon

Astronomy 111

Page 2: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Motions of the Earth

Page 3: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Stars, Sun, Moon and planets move in counterclockwise circles around north (south) celestial pole.

Objects generally move east to west when above the horizon (“rising” in east, “setting” in west).

What causes these circular motions?

Observation:

Page 4: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Motions of the Earth

•  The Earth rotates on its axis

•  This motion causes: •  Sunrise and

sunset •  Motion of stars

Page 5: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Stars rise and set

Page 6: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

•  One star in the sky never moves –  the “North Star” or Polaris

•  Why is Polaris fixed in position?

Page 7: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Earth’s axis is fixed

Page 8: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Where was this

picture taken?

Page 9: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Celestial navigation made simple

At Earth’s North Pole: Polaris is directly overhead

At Earth’s Equator: Polaris is due north, on the horizon

In Earth’s Northern hemisphere: Polaris is due north - height above the horizon (in degrees) is equal to your latitude (in degrees)

Page 10: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Earth’s rotation causes apparent motion

•  Remember: the stars and Sun DO NOT orbit the Earth once per day

•  Rather, the Earth rotates once per day – Produces apparent motions of stars, Sun,

planets

Page 11: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The celestial sphere

Page 12: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Thinking about the stars we see in the night sky

The celestial sphere

Page 13: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The celestial sphere: a large imaginary sphere around Earth

Page 14: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Special locations on the celestial sphere

North Celestial Pole = point directly above Earth’s North Pole (near the star Polaris)

South Celestial Pole = point directly above Earth’s South Pole (no nearby bright star)

Celestial Equator = circle directly above Earth’s Equator

Page 15: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Locations on celestial sphere

Page 16: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Distances between points on the celestial sphere are measured in degrees, arcminutes, and arcseconds

360 degrees in a circle 60 arcminutes in a degree 60 arcseconds in an arcminute

½ degree = angular size of Sun & Moon

Page 17: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The night sky

Page 18: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The sky is divided into 88 constellations

•  Mesopotamia, circa 3000 BC: oldest know constellations

•  Ptolemy, 2nd century AD: 48 constellations in northern sky

•  16th to 18th century AD: unmapped (mostly southern) regions of sky filled in –  Telescopium, Microscopium, Reticulum!

Page 19: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Modern usage still retains names of stars and rankings by brightness within a constellation, although Arabic names are also used for the

brightest stars

Hipparchus

Hipparchus (ca. 140 BC) was perhaps the greatest astronomer of ancient times. He produced a catalogue of 1000 stars and classified them according to

their apparent brightness.

Page 20: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Constellations are arbitrary

Other cultures, other constellations:

Stars in a constellation usually are not at the same distance from us.

At a different place in our Galaxy, we would see different star patterns.

Emu Southern

Cross

Page 21: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

Sun moves west to east relative to stars (about 1 degree per day).

What causes this annual motion?

Page 22: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Two possible explanations of 1 year cycle:

HYPOTHESIS #1 Sun revolves around

Earth at a slightly slower rate than the

celestial sphere.

WRONG!

HYPOTHESIS #2 Earth revolves around

the Sun, once per year.

RIGHT!

Page 23: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

A model of the

celestial sphere,

showing the

constellation

borders, the

celestial equator,

and the apparent

path of the Sun

against the

background of

constellations.

Page 24: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Sun appears to move west to east relative to stars (1 year cycle)

Today the Sun is “in” a particular constellation, next month in a different one, etc.

Sun’s path on the celestial sphere = ecliptic

Constellations through which the ecliptic runs = zodiac

The ecliptic is NOT the same as the celestial equator!

Page 25: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Sun is in the direction of the constellation

Virgo in September, as

viewed from the Earth.

That is why people born in September are said to be born

under the astrological

sign of Virgo.

The Zodiac

Page 26: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

The weather in the summer is hotter than in the winter (especially in Texas!)

What is the cause of the seasons on Earth?

Page 27: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Remember that the Earth's axis of rotation is tilted 23.5 degrees

to the plane of its orbit about the Sun.

Earth’s tilt causes seasons

Page 28: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Earth’s tilt causes seasons

Page 29: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

When the northern hemisphere is tilted towards the

Sun we have summer in the northern hemisphere and

winter in the southern hemisphere.

When the northern hemisphere is tilted away from

the Sun we have winter in in the northern hemisphere

and summer in the southern hemisphere.

This is the cause of the seasons.

Earth’s tilt causes seasons

Page 30: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Earth’s tilt causes seasons

Page 31: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The reason it is warmer in summer than in winter

is that the sunlight is more concentrated on the

ground when the Sun is higher in the sky.

Earth’s tilt causes seasons

Page 32: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The first day of spring occurs about March 20th or March 21st.

(In the Northern hemisphere, this is called the vernal equinox.)

The first day of autumn occurs about September 22nd. (This would be the first day of spring in

The Southern hemisphere, and the autumnal equinox in the Northern hemisphere.)

The key thing is that the equinoxes occur when the declination of the Sun is zero degrees (i.e.

located on the celestial equator).

Seasons

Page 33: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

“Observation”:

The location of Polaris moves (over thousands of years)… the North Star was not always the North Star!

What causes this motion?

Page 34: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Spinning top takes <1 sec!

to precess...!

Earth takes 26,000 years!!

Precession

Page 35: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Hipparchus compared the coordinates of some stars with records made by the Babylonians and discovered that the ecliptic longitudes of the stars were increasing with time, about 1 degree per century. (The modern value is about 1 degree in 72 years.) This is called precession (not to

be confused with the word “precision”). The Earth turning on its axis is like a spinning top.

Precession

Page 36: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Precession

While Polaris is close to the north celestial pole now, it was not always the case. Due to the 26,000 year period of precession, many stars take their turns being the pole star.

Page 37: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

•  There is a large bright object in the nighttime (and daytime) sky

•  How does the Moon move?

Page 38: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Motions of the Moon

Page 39: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Moon appears to move west to east relative to stars (1 month cycle)

Today the Moon is “in” some constellation

In two weeks: something different In four weeks: first one, again.

Observation: Moon moves west to east relative to stars, taking 27.3 days to complete cycle.

What causes this monthly motion?

Page 40: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Explanations of 1 month cycle:

HYPOTHESIS #1 Moon revolves around Earth at a

significantly slower rate than the

celestial sphere.

WRONG!

HYPOTHESIS #2

Moon revolves around Earth, once

per month.

RIGHT!

Page 41: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

(not to scale)!

The Moon’s orbit

Page 42: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Phases of the Moon

•  The moon’s phases are due to its motion relative to the Earth and Sun

Page 43: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Page 44: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

•  Both the Sun and the Moon may be eclipsed in their orbits

•  We live in a very special place in order for this to happen…

Page 45: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Solar eclipses

Page 46: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Solar eclipses

Solar eclipses occur when Moon is between Sun and Earth.

Solar eclipses occur at NEW MOON.

Page 47: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Total Solar Eclipse:

Page 48: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Solar Eclipses

Only a small part of the earth observes a Total Solar Eclipse!

Page 49: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Total Lunar Eclipse

Page 50: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Lunar eclipse

Lunar eclipses occur when Earth is between Sun and Moon.

Lunar eclipses occur at FULL MOON.

Page 51: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Solar vs. Lunar eclipses

Total solar eclipse is visible from a narrow path (up to 270 km wide) for a short time (up to 7.5 min).

Total lunar eclipse is visible from half the Earth.

From Texas, next total lunar: Dec 21, 2010; next total solar: Apr 8, 2024

Page 52: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Page 53: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Observation:

•  The level of the ocean at the seashore rises and falls at different times during the day

•  What causes tides?

Page 54: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Tides are caused by the difference between the Moon’s gravitational force on different sides of the Earth

Time between high tides = 12 hours,

25 min Time between moonrises = 24 hours, 50 min

Page 55: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Tides

The gravitational force between two objects decreases as the distance between them increases.

The Moon’s gravitational pull on an object will be 7% greater on the closer side of the Earth than on the further side.

Page 56: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

If the Moon’s pull were constant, then Earth would be undistorted.

After subtracting average pull, Earth is stretched in Moon’s direction.

Result: TWO tidal bulges, on opposite sides of Earth.

Tides

Page 57: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Why do we notice tides at the seashore?

Rock is stiff: Tidal bulges in rock are only 0.3 m high.

Water is fluid: Tidal bulges in water are 1 meter high.

Water bulges rise above rock bulges.

Page 58: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Sun also creates tides on Earth

High tides are highest when Sun, Earth and Moon line up (called ‘spring tide’).

High tides are lowest when Sun, Earth & Moon are at right angles (‘neap tide’).

Page 59: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Tidal forces are slowing the Earth’s rotation and enlarging the Moon’s orbit

The ocean’s tidal bulges press down on the ocean floor.

Friction robs energy from Earth’s rotation and uses it to heat the ocean.

This process is known as “tidal breaking”. (Think of the tidal bulges as brake pads!)

The length of the day is increasing by 0.002 seconds per century.

Page 60: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Moon rotates about its axis as it revolves around the Earth

On Earth, we always see the same side of the Moon (“near side”).

The “far side” is always turned away from us.

Page 61: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

The Man in the Moon

Moon creates tidal bulges on Earth: Earth creates BIGGER bulges on Moon.

The Moon has already undergone tidal braking.

The Moon’s rotation has slowed to the point where its rotation period equals its orbital period.

This is why the Moon always keeps the same side turned to us.

Page 62: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

ASTR111 Lecture 2

Goodbye Moon

Friction between the tidal bulges and ocean floor drags the bulges in the direction of the Earth’s rotation.

Bulges lead Moon by about 10 degrees.

The leading bulge steadily tugs the Moon into a larger orbit.

The average Earth-Moon distance is increasing by 4 meters per century.

Page 63: Lecture 2: Motions of the Earth and Moonpeople.physics.tamu.edu/depoy/astr111TR/Notes/lecture2.pdfASTR111 Lecture 2 Tidal forces are slowing the Earth’s rotation and enlarging the

How do we know the distance is increasing?

Measure the distance to the moon with great accuracy and watch it change!

Lunar Laser Ranging Experiment

(1969, Apollo 11)

Goodbye Moon