Chp 2 - Motions of Earth
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Transcript of Chp 2 - Motions of Earth
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Chapter 2
Patterns in the
SkyMotionsof Earth
2013 W.W. Norton & Company, Inc.
21st CENTURYASTRONOMY
FOURTHEDITIONKay | Palen | Smith | Blumenthal
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!
Our focus: Earths daily rotation.
Earths annual orbit.
The Moons monthly
orbit.
Consequences of therelationship/alignment
of Earth, the Moon,
and the Sun (phasesof the Moon,
eclipses).
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! Constellationsare arbitrary patterns of stars
in the sky.
! Culturally important products of human
imagination.
!
Ancient cultures built structures to study themand other astronomical phenomena.
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!
Just because stars are grouped in the sameconstellation does not mean they are near
each other in space.
! Some stars move in different directions.
! The constellations slowly change shape on
timescales larger than human lives.
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!
As viewed from abovethe North Pole, Earth
rotates (spins)
counterclockwise on
its axis.
! One rotation takes
24 hours.
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!
Celestial sphere:projection of Earths
axes and equator ontospace.
!
A useful fiction.! Points on the sphere
correspond to directions,not distances.
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!
Celestial sphere rotatesaround the northand
southcelestialpoles
once each day.
!
Celestial equator:midway between.
! Ecliptic: path of the
Sun, inclined 23.5degrees to celestial
equator.
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!At Earths north pole, you would see half the
celestial sphere.
! The north celestial pole is directly overhead.
! Stars rotate counterclockwise in 24 hours.
! No star rises or sets: all are circumpolar.
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!At the equator, all stars rise and set.
! The celestial poles are on the northern
and southern horizons.
! Observers can see the whole celestial sphere
as it rotates.
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! At an intermediate latitude, one pole is above the horizon.
!
The angle to the horizon from that pole equals the latitude.
! Some stars are circumpolar.
! Some stars rise and set.
! Some stars are never visible.
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The Size of Earths Orbit
! The average distance of Earth to the Sun is
called the astronomical unit, or AU.
! 1 AU = 150 million km.
! Earth revolves counterclockwise around the
Sun as viewed from above.
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!
The Suns motion on the ecliptic reflects Earthsorbit around the Sun.
! Earth revolves around the Sun once a year.
!As Earth moves, the Sun is seen against
different constellationsthe zodiac.
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Earths Axis
!
Earths axis is not perpendicular to the eclipticplane.
! Instead, it is at an angle of 23.5 degrees.
! This is why there are seasons.
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Earths Axis
! The angle of sunlight is closer toperpendicular in summer.
! Energy is more concentrated.
! The southern hemisphere is opposite the
northern hemisphere.
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! Earths obliquityof 23.5 is the reason for
the seasons.
! If the tilt were larger or smaller, life would
most likely be different due to the difference
in seasonal variation.! The differences in climate over the surface of
Earth have resulted in a broad diversity of
life, specifically adapted to those locations.! The changes in climate over the course of the
year most likely greatly influenced the
behavior of life, including migratory patterns.
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Special Days of the Year
!
Summer solstice: Sunfarthest north.
! Autumnal equinox: Sun
on the equator, moving
southward.
! Winter solstice: Sun
farthest south.
!
Vernal equinox: Sun onthe equator, moving
northward.
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Credit: Robert Polzl Credit: Tunc Tezel
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Precession
!
Currently, the northcelestial pole is near
the bright star
Polaris.
!
Earths axis wobbleswith a period of
26,000 years.
!
Location of the polesslowly shifts.
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!
Earth wobbles like a top, slowly.! Since the axis shifts, the equator shifts.
! Positions of the equinoxes precess as well.
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The Moon
What causes moon phases?
Why do we only see one side of the Moon?
How are tides generated?
How do eclipses work?
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1/4ththe diameter of Earth
1/50 the volume of Earth
1/81stthe mass of Earth
1/6ththe gravity of Earth
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Average distance ~ 235,000 miles (385,000 km)
(Earth, Moon, and their separation are scaled in the above
animation. The yellow line represents the scaled speed of light.)
Moons orbital eccentricity - 0.0549
Perigee 363,000 km, Apogee 405,000 km
42,000 km distance change Moon can change in size by ~10%
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The side shaded red is the side we observe from Earth.
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Phases of the Moon
!
The Moon shinesbecause of reflected
sunlight.
! Half of the Moon
is always bright.
! The phase is
determined by how
much of the brightside we see.
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Phases of the Moon
!
New moon: moonbetween Earth andthe Sun.
! Waxingcrescent.
!
Quarter moon:moon at rightangles with Earthand the Sun.
!
Waxing gibbous.! Full moon: moon
on opposite sideof Earth from Sun.
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Phases of the Moon
!
After a full Moon,the amount ofbrightness beginswaning.
!
In the northernhemisphere, theMoon fills in fromright to left and also
fades out from rightto left.
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Orbital Period of the Moon
!
The Moon takes 27.3days to orbit once with
respect to the stars
(sidereal period).
!
Lunar phases repeatevery 29.5 days (synodic
period).
!
The Moons rotationalperiod equals its sidereal
period.
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! Throughout history, humans have made
calenders based on the seasons (withrespect to the Sun) or the Moons cycle of
phases.
!
The number of calendar days (365) does notfit neatly into months (29.5 days) or years
(365.24 days).
! Humans creatively made calendars to deal
with this.
! Today the Gregorian calendar,which
includes leap years to keep it on track, is
used.
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Solar Eclipses
!
Solar eclipses happen at new Moon.! Moon passes between Earth and the Sun.
! Only a small portion of Earth can witness
each one.
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!
Three types of solareclipses:
Total: The Mooncompletely blocks
the Suns light. Partial: Only part
is blocked.
Annular: The Sun
appears as a brightring surrounding the
Moon.
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! The part of the Moons shadow you are in
determines which type of solar eclipse you
see.
! Umbra: Total or annular.
!
Penumbra: Partial.
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! Lunar eclipses happen at fullMoon.
! Earth is between the Sun and theMoon.
! Visible over a wider area of Earth.
!
Last a lot longer than solareclipses.
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! Eclipses do not occur every month because
the Moons orbit is tilted 5.2 with respect toEarths orbit around the Sun.
! Intersection: line of nodes.
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