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The Sun-Earth-Moon System

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[This is calculated by dividing the circumference of the Earth at the equator (about 24,900 miles or 40,070 km) by the number of hours in a day (24).] – PowerPoint PPT presentation

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Title: The Sun-Earth-Moon System


1
The Sun-Earth-Moon System
  • Rotation
  • Coriolis Effect
  • Tides
  • Revolution
  • Seasons
  • Moon
  • Lunar Eclipse
  • Solar Eclipse

2
Rotation
23.5
  • Earth is a round, 3-dimensional sphere
  • AXIS imaginary vertical line around which earth
    spins
  • 23.5 from vertical

3
Rotation
  • ROTATION
  • the spinning of Earth around its axis

4
Rotation
  • Effects of ROTATION
  • Night and day plants, animals, and people
  • Daily change in temperature

5
  • Effects of ROTATION
  • Earth bulges at the equator

Polar diameter 7900 miles (12,714
km) Equatorial diameter 7927 miles (12,756 km)
6
Rotation
  • How fast is the Earth spinning around its axis?
  • At the equator, the Earth's surface moves 40,070
    kilometers in 24 hours. That is a speed of about
    1040 miles/hr (1670 km/hr or 0.5 km/sec).
  • This is calculated by dividing the circumference
    of the Earth at the equator (about 24,900 miles
    or 40,070 km) by the number of hours in a day
    (24).
  • As you move toward either pole, this speed
    decreases to almost zero (since the circumference
    of the spinning circle at the extreme latitudes
    approaches zero).

7
Rotation
  • Effects of ROTATION
  • CORIOLIS EFFECT
  • Earth rotates at different speeds at different
    latitudes
  • Any moving solid, liquid , or gas is turned to
    the RIGHT of its intended path in the Northern
    Hemisphere
  • Any moving solid, liquid , or gas is turned to
    the LEFT of its intended path in the Southern
    Hemisphere
  • Winds
  • Ocean currents

8
  • Effects of ROTATION
  • CORIOLIS EFFECT

9
  • Effects of ROTATION
  • CORIOLIS EFFECT

http//topex-www.jpl.nasa.gov/aviso/graphics/gener
al/outreach/tutorial/coriolis.mov
10
  • Effects of ROTATION
  • CORIOLIS EFFECT

11
Rotation
  • Effects of ROTATION
  • Tides
  • The gravitational pull of the moon and the sun
    produces a rhythmic rise and fall of the oceans
    as the Earth rotates

12
Tides
  • Effects of ROTATION
  • Result of the gravitational attraction between
    the Earth, sun, and moon.
  • As the moon rotates around the Earth, it pulls
    the water on the nearest side of the Earth
    outward into a bulge.
  • A similar bulge on the opposite side of the Earth
    is caused by inertia - gravitational attraction
    of the moon is less water furthest away than on
    the Earth.

13
TIDES
  • SPRING TIDE
  • NEAP TIDE

14
TIDES
  • SPRING TIDE
  • During time of the new moon and full moon, the
    sun and moon are in a straight line
  • Combined gravitational pull produces spring tides
  • High tides are very high and low tides are very
    low.

15
TIDES
  • NEAP TIDE
  • When sun and moon are at right angles from the
    Earth, during the quarter phases of the moon
  • Gravitational pull on the oceans is less
  • A smaller difference between high and low tide

16
TIDES
Nova Scotia's Hall's Harbour at high tide.
  • The tides have a vertical difference, between
    high and low tide, of up to 14 metres (48 feet)!

And at low tide just six hours later.
17
TIDES - WAVES
  • Tides are due to GRAVITATIONAL ATTRACTION NOT wind

18
TIDES
  • A review of tides and the position of the sun and
    moon

19
Revolution
  • REVOLUTION Earths yearly orbit around the Sun
  • 365.25 days
  • Earths orbit is an ellipse
  • Distance between the Earth and Sun changes during
    the year because the orbit is not a circle!
  • Average distance is 150,000,000 km
  • Earths tilt on its axis remains in the same
    direction!

20
Revolution
NOTE This is not to scale in reality, the sun
is a lot bigger to scale, and Earth is a lot
further away.
21
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22
Seasons
  • CAUSES of SEASONS
  • Tilt of the Earths axis
  • Uneven heating of Earths surface
  • The hemisphere tilted toward the Sun receives
    more solar energy
  • Revolution of the Earth around the sun

23
Seasons
24
Seasons
  • Solstice
  • Day when the sun reaches its greatest distance
    north or south of the equator
  • Northern Hemisphere
  • SUMMER June 21 or 22
  • WINTER December 21 or 22

25
Seasons
  • Equinox
  • Day when the sun is directly over the equator
  • Daylight and nighttime are equal
  • Northern Hemisphere
  • SPRING (Vernal)
  • March 21or 22
  • FALL (Autumnal)
  • September 21 or 22

26
Seasons
27
College of Alameda Physical Geography
http//members.aol.com/pakulda/emmod.htm
28
MOON
  • A cold, rocky body about 2,160 miles (3,476 km)
    in diameter.
  • It has no light of its own - shines by sunlight
    reflected from its surface.

29
MOON
  • Rotates on its axis
  • Rotation of the moon takes about as long as its
    revolution
  • Revolves around the Earth
  • once every 27? days
  • The same side of the moon is facing the Earth

30
Phases of the MOON
  • WAXING
  • When the moon is between New and Full
  • Portion of moon visible is INCREASING
  • WANING
  • When the moon is between Full and New
  • Portion of the moon visible is DECREASING

31
PHASES OF THE MOON
The photographs show what the moon looks like
from Earth. The drawings show what the moon would
look like from space.
32
Lunar Eclipse
  • Earths shadow falls on the moon
  • can only occur at Full Moon
  • UMBRA darkest part of the shadow, a region
    where the Earth blocks all direct sunlight from
    reaching the Moon.
  • PENUMBRA cone of shadow cast by deflected
    light, a zone where the Earth blocks part but not
    all of the Sun's rays from reaching the Moon

33
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34
Lunar Eclipse
  • There is a full moon once a month why not a
    lunar eclipse?
  • All 3 bodies must be in perfect alignment
  • Must be nighttime when alignment occurs, only
    half the planet is experiencing night at a given
    time
  • During Full Moon phase, the moon usually passes
    above or below Earth's shadows and misses them
    entirely. No eclipse takes place.
  • Two to four times each year, the Moon passes
    through some portion of the Earth's penumbral or
    umbral shadows resulting in an eclipse

35
MOON
Earths orbit around the sun
  • The moon's orbital plane does not "lie flat"
    along the ecliptic, but forms an angle of about
    5º - affects chances of experiencing an eclipse.
  • (note the distances in this diagram are not to
    scale)

36
MOON
Path of moon through Earths shadow during total
eclipse in 2000.
Note the moon does not pass directly through the
center of the UMBRA
37
LUNAR ECLIPSE
  • Partial Lunar Eclipse
  • A portion of the Moon passes through Earth's
    umbral shadow.
  • These events are easy to see, even with the
    unaided eye.
  • Total Lunar Eclipse
  • The entire Moon passes through Earth's umbral
    shadow.
  • These events are quite striking for the vibrant
    range of colors the Moon can take on during the
    total phase (i.e. - totality).

38
LUNAR ECLIPSE
  • When an eclipse of the Moon takes place, everyone
    on the night side of Earth can see it.
  • About 35 of all eclipses are of the penumbral
    type which are very difficult to detect, even
    with a telescope.
  • 30 are partial eclipses which are easy to see
    with the unaided eye.
  • 35 or so are total eclipses, and these are quite
    extraordinary events to behold.

39
LUNAR ECLIPSE
  • Indirect sunlight still manages to reach and
    illuminate it.
  • However, this sunlight must first pass deep
    through the Earth's atmosphere which filters out
    most of the blue colored light.
  • The remaining light is a deep red or orange in
    color and is much dimmer than pure white
    sunlight.
  • Earth's atmosphere also bends or refracts some of
    this light so that a small fraction of it can
    reach and illuminate the Moon.

40
LUNAR ECLIPSE
  • If the Earth had no atmosphere, then the Moon
    would be completely black during a total eclipse.
    Instead, the Moon can take on a range of colors.
  • The filtering and refracting effect of Earth's
    atmosphere makes the total phase of a lunar
    eclipse interesting.
  • The exact appearance depends on how much dust and
    clouds are present in Earth's atmosphere.
  • Major volcanic eruptions tend to make total
    eclipses very dark, since these events dump large
    amounts of ash into Earth's atmosphere.
  • During the total lunar eclipse of December 1992,
    dust from Mount Pinatubo rendered the Moon nearly
    invisible.

41
SOLAR ECLIPSE
  • Moon moves directly between Earth and the sun
  • UMBRA Dark inner shadow total eclipses are
    seen from within this shadow. The track of the
    Moon's shadow across Earth's surface is called
    the Path of Totality. It is typically 10,000
    miles long but only 100 miles or so wide.
  • PENUMBRA Faint outer shadow partial eclipses
    are seen from within this shadow.

42
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43
SOLAR ECLIPSE
  • There is a NEW moon once a month why not a
    solar eclipse?
  • All 3 bodies must be in perfect alignment
  • During New Moon phase, the moons shadow usually
    passes above or below our planet and misses Earth
    entirely. No eclipse takes place.
  • At least twice each year, the 3 bodies line up so
    that some part of the moons shadow falls on
    Earths surface
  • An eclipse of the Sun is seen from that region

44
SOLAR ECLIPSE
2000 Jul 31 Partial Solar Eclipse http//sunearth
.gsfc.nasa.gov/eclipse/OH/OH2000.html
45
QUESTIONS
  • Describe the two types of planetary motion.
  • Why does the Earth have tides?
  • What is the relationship between tides and waves?
  • What are the characteristics of a wave?
  • What causes the Coriolis Effect? What is the
    Coriolis Effect?
  • Why does the Earth have seasons?
  • What is the difference between a solstice and an
    equinox?

46
QUESTIONS
  • What is the difference between a solar eclipse
    and a lunar eclipse?
  • When can you see a total solar eclipse? A total
    lunar eclipse?
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