1 Telling Time A Warm Up Exercise The ecliptic is a) The annual path of the Earth across the celestial sphere b) The extension of the Earth’s equator c) The annual path of the Sun across the celestial sphere d) When the moon covers the sun A Warm Up Exercise In Columbus, the longest night of the year occurs close to the a) Fall Equinox b) Summer Solstice c) Spring Equinox d) Winter Solstice A Warm Up Exercise In Columbus, the longest night of the year occurs close to the a) Fall Equinox b) Summer Solstice c) Spring Equinox d) Winter SolsticeKeeping track of Time • All of our time-keeping conventions are astronomically based: – Years are based on the apparent annual solar motion due to the Earth’s orbit around the Sun. – Months are based on the cycle of the Lunar Phases (“Month” derives from “Moon”). – Days are based on the apparent daily solar motion as the Earth rotates on its axis. Dividing the Day • We divide the Day into 24 equal hours, with each day beginning at midnight. • This wasn’t always the case: –The day began at dawn (sunrise). –Equal division of Day and Night into 12 hours. –The length of the hour was different for day and night (except at the Equinoxes). • Worked fine for sundials.
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Telling Time
A Warm Up Exercise
The ecliptic is
a) The annual path of the Earth across the celestial sphere
b) The extension of the Earth’s equator
c) The annual path of the Sun across the celestial sphere
d) When the moon covers the sun
A Warm Up Exercise
In Columbus, the longest night of the year occurs close to
the
a) Fall Equinox
b) Summer Solstice
c) Spring Equinox
d) Winter Solstice
A Warm Up Exercise
In Columbus, the longest night of the year occurs close to
the
a) Fall Equinox
b) Summer Solstice
c) Spring Equinox
d) Winter Solstice
Keeping track of Time
•All of our time-keeping conventions are
astronomically based:
– Years are based on the apparent annual solar motion
due to the Earth’s orbit around the Sun.
– Months are based on the cycle of the Lunar Phases
(“Month” derives from “Moon”).
– Days are based on the apparent daily solar motion
as the Earth rotates on its axis.
Dividing the Day
•We divide the Day into 24 equal hours, with each day beginning at midnight.
•This wasn’t always the case:
–The day began at dawn (sunrise).
–Equal division of Day and Night into 12 hours.
–The length of the hour was different for day and night (except at the Equinoxes).
•Worked fine for sundials.
2
Equal Hours
•The invention of mechanical clocks in the 1300s led to a need for equal hours:
–Ensured the clocks read true in the morning.
–Simplified clock design.
•Medieval clocks were large and complex:
–Erected in towers in cities for everyone to see.
–Led to a standardization of time keeping
–Personal timepieces came only later.
Oldest surviving clock in
England – Salisbury
Cathedral (1386)
These clocks were used
only to chime bells (no
hands) and were only
accurate to about 30
minutes per day
Dividing the Hour
•Until 1500s, clocks only kept time to the quarter hour.
•Further division of the hours was needed as clocks became more complex.
–1 hour was divided into 60 minutes.
–1 minute was divided into 60 seconds.
•Seconds didn’t become common until the 1670s (39-inch pendulum clocks).
Solar Time
•The Day is measured using the Sun.
•Local Solar Noon:
–Occurs when the Sun is on your meridian.
•Mean Solar Day:
–The time between successive Noons.
•Noon depends on your longitude:
–Person 15º east of you sees noon 1 hour earlier.
–Person 15º west of you sees noon 1 hour later.
Sidereal Time
• Sidereal Time is measured relative to the “fixed stars”.
• As the Earth rotates through 1 day, it moves about 1º
along its orbit around the Sun.
–As seen with respect to the stars, the Earth has move for an
extra 4 minutes in order for the Sun to return to the observer’s
meridian (noon).
• Stars rise 4m earlier each night measured against solar
(civil) clocks.
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NoonT=0h
T=23h 56m 04s
(Sidereal Day)
T=24h
(Solar day)
Not to Scale
Standard Time
•Invention of long-distance railroads and telegraph networks required standardized time keeping:
– Coordination of interstate railroad schedules.
– Telegraph lines linked many widely separated longitudes instantaneously, but needed to coordinate them.
•Small differences in local solar time began to matter.
Time Zones
•Charles Dowd (1883):
– Divided the Earth into Time Zones by longitude from the Prime Meridian.
– Basic time zones are 15º of longitude apart (360º/24h = 15º/hour)
– Each time zone keeps local solar time for a fixed reference longitude.
– All longitudes within that zone use “Zone Time”instead of local solar time.
The Motion of the Moon
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A Warm Up Exercise
The ecliptic is
a) The annual path of the Earth across the celestial sphere
b) The extension of the Earth’s equator
c) The annual path of the Sun across the celestial sphere
d) When the moon covers the sun
SCP
NCP
CEq
Winter
Solstice
Summer
Solstice
Vernal
Equinox
Autumnal
Equinox
“O! Swear not by the moon, the inconstant moon
That monthly changes in her circled orb,
Lest that thy love prove likewise variable.”
William Shakespeare,
Romeo & Juliet, II, 2
Our Nearest Celestial Neighbor
•The Moon is a natural satellite of the Earth.
•Its orbit around the Earth is elliptical:
–~5% deviation from circular.
–The orbit is tilted by 5º from the Ecliptic.
•Mean Distance: 384,400 km
–Perigee (Closest Approach): 363,300 km
–Apogee (Maximum Distance): 405,500 km
–Appears ~11% larger at Perigee than at Apogee
The Moons Orbit is Elliptical
(closest point on orbit)/(furthest point on orbit) = 0.9
Which means the angular size of the moon changes by the same factor since
(angular size)=(moon diameter)/(distance)
It will be 11% bigger at perigee (closest approach) than apogee (most distant point).
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Synchronous Rotation
•The Moon rotates at the same rate it revolves:
• Completes 1 rotation in the same time it takes to complete 1
orbit (revolution) around the Earth.
•Always keeps the same face towards us.
• Near Side: hemisphere facing towards us
• Far Side: hemisphere facing away from us
•Caused by tidal coupling between the Earth and Moon.
• The Moon is “tidally locked” to the Earth
•Example of a “resonance”
Lunar Near Side
Full Moon(Lick Observatory Photo)
Lunar Far Side
Historic image returned
by the Soviet Luna 3
Spacecraft in October 1959.
Lunar Far Side
Far-side image
returned by the Galileo
Spacecraft during a fly-by
enroute to Jupiter (Dec 1990)
Case I – The Moon Is Not Rotating
start ¼ orbit
½ orbit¾ orbit
Case II – Tidal Locking -- The Moon Spins as Fast
as It Orbits
start ¼ orbit – moon rotated by 90o
Moon rotating in the
same direction and at
the same rate as the
orbit
¾ orbit – moon rotated by 270o½ orbit – moon rotated by 180o
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Why is it called “Tidal Locking”?
The “tidal locking,” as the name suggests, is a result of the tidal
effects produced by the Earth on the Moon
If the Moon were rotating faster or slower, the Earth would
produce time varying tidal deformations in the moon.
These deformations produce frictional forces that either slow the
rotation rate (if rotating faster than synchronously) or speed up the
rotation rate (if rotating slower than synchronously)
When tidally locked, the tidal deformations do not vary with time
so there is no friction and the rotation rate stops changing
The Moon’s Orbit Is Slowly Expanding
It expands by 3.8 cm per year
Phases of the Moon
•The Moon produces no visible light of its own
– It shines only by reflected sunlight
– Surface is very dark, only ~7% reflective
•During the month, we see a complete cycle of Phases:
– The sunward hemisphere is fully lit.
– The opposite hemisphere is dark.
– The phase of the Moon is the fraction of the sunlit hemisphere
visible to us.
New Moon Full Moon
Waning Crescent
Last Quarter
Waning Gibbous
Waxing GibbousWaxing Crescent
First Quarter
The Moon’s Phases
EarthThis Way
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New & Full Moon
•New Moon:
–Moon and Sun are on the same side of the sky.
–Near side is in total darkness.
–Moon and Sun rise together.
•Full Moon:
–Moon is opposite the Sun in the sky.
–The near side is fully illuminated.
–Moon rises as the Sun sets.
Quarter Moon
•Earth, Moon, & Sun are at right angles:
–Half of the near side is illuminated
–Half of the far side is illuminated
•First Quarter:
–Between New Moon and Full Moon.
•Last Quarter:
–Between Full Moon and New Moon.
Waxing & Waning
•Waxing: increasing illumination
–Waxing Crescent: after New Moon
–Waxing Gibbous: just before Full Moon
•Waning: decreasing illumination
–Waning Gibbous: just after Full Moon
–Waning Crescent: before New Moon
What you can see strongly depends on the phase
For a 1st quarter moon, for example, the moon will always be
visible at sunset, and then sets at midnight (it rose at noon).
Moonrise, Moonset...
•You don’t see all moon phases at all times
–Never see a crescent moon at midnight.
–Never see the last quarter moon at sunset.
–Never see a full moon during the day.
•Times of rising and setting depend on the Earth-
Sun-Moon configuration as viewed from the
surface of the rotating Earth.
•When in doubt, draw a picture!
The View from the Moon
•Question:
What would an astronaut on the Lunar near side see
during one month?
•Answer:
– See the Earth neither rise nor set, but stay nearly
fixed at the same position in the sky.
– See the Earth rotate on its axis once every 24h.
– See the Earth go through phases.
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The earth as viewed from the Apollo 17
landing site in the Taurus-Littrow valley.
Earth Phase Movie
https://www.youtube.com/watch?v=YQfm2icwtDk
Sidereal Period
•The time for the Moon to complete one orbit around the
Earth with respect to the stars.
–Moon’s Sidereal period = 27.3 days
–Also called the “Sidereal Month”
•Measure by watching its motions against the
background stars – returns to the same constellation
•The phase at the end of a sidereal month is DIFFERENT