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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