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Climate and Latitude QuickTime™ and aTIFF (Uncompressed) decompressorare needed Sun’s rays spread over large area = cooler concentrate in small area = warmer Warmest where sun directly overhead (at noon) cooler warmer cooler

Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

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Page 1: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Climate and Latitude

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• Sun’s rays – spread over large area = cooler– concentrate in small area = warmer– Warmest where sun directly overhead (at noon)

cooler

warmer

cooler

Page 2: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Seasons

• What do we observe?– Warm in Summer; Cold in Winter– Yearly cycle

• Linked to Sun’s location on ecliptic(Spring = Vernal Equinox, Summer = Summer Solstice; etc)

• Sun is heat source

– Seasons in N and S hemispheres opposite• N summer = S winter

– Seasons near Equator less severe

Page 3: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Cause of Seasons• Changing distance to Sun?

– Orbit is ellipse; distance changes– Good idea, BUT

• Orbit almost circular– Trivial change in distance– little change in heating

• Closest to sun in January– Predicts summer in January

• Both N and S hemispheres at same distance– Predicts seasons same in N and S hemispheres

No!

Page 4: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Cause of Seasons• Tilt of Earth’s Axis?

– Location where sun overhead (at noon)• Vernal & Autumnal Equinoxes (Mar 21, Sept 21)

– Overhead at Equator

• Summer Solstice (Jun 21)– Overhead on Tropic of Cancer (23.5º N)– Warmer in N hemisphere; cooler in S hemisphere

• Winter Solstice (Dec 21)– Overhead on Tropic of Capricorn (23.5º S)– Warmer in S hemisphere; cooler in N hemisphere

Yes

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cooler

cooler

warmer

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Zen

ith Zenith

Horizon

Hor

izon

Page 5: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Cause of Seasons - Part 2• Tilt of Earth’s Axis?

– Path of Sun in sky• Summer Solstice (Jun 21)

– Sun farthest north– Transits high at noon– Days are long

• Winter Solstice (Dec 21)– Sun farthest south– Transits low at noon– Days are short

Large amount of heating

Small amount of heating

Yes

Page 6: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

For an observer in the continental U.S., which, if any, of the x’s (a – e) in the figure below correctly shows the position of the Sun’s shadowat noon? Note that the position of the Sun’sshadow at noon on the Winter and Summer Solstices are shown.a) ab) bc) cd) de) e

Page 7: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Motions and Phases of the Moon

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Composite Image Credit: T.A. Rector, I.P. Dell'Antonio, NOAO, AURA, NSF

Page 8: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Motion of Moon• Daily Motion Like Stars

– Rise in East; Transit in South; Set in West

• Moon Orbits Earth– Moon slips on Celestial Sphere

• 13 degrees per day = 1 lunar diameter per hour

– Sidereal Period = Orbital Period • 27.3 days

– Time from full moon to full moon• 29.5 days(similar to sidereal day vs. solar day)

– Moon rises roughly 50 min later each day

Page 9: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Rotation of Moon

• Always see same side– Moon rotates once per month

Non-rotating moon

Rotating moon

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Page 10: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Moon Phases• New = all black

• Full = all white

• Crescent < half white

• Gibbous > half white

• Quarter = half white

• Waxing = growing

• Waning = shrinking

crescent

crescent

gibbous

gibbous

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QuickTime™ and aTIFF (Uncompressed) decompressorare needed to see this picture.1st quarter

full

3rd quarter

Wax

ing

Wan

ing

D --> O --> C

Page 11: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Phases of Moon

Page 12: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Phases of Moon

• Not caused by Earth’s shadow!• Cause:

– Changing view of illuminated side (as Moon orbits Earth)

• “Back Side” sometimes called “Dark Side”– Back side not dark– Back side has night and day

(just like front side)

Page 13: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Workbook Exercise: Cause of Moon Phases(pages 23-25 in workbook)

Page 14: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

• During the full moon phase, how much of the Moon’s surface is being illuminated by sunlight?

a) noneb) less than halfc) halfd) more than halfe) all

Page 15: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Workbook Exercise: Predicting Moon Phases(pages 27-28 in workbook)

Page 16: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

• Which phase of the Moon rises at noon?a) Waning gibbousb) Third quarterc) First quarterd) Waxing crescente) None of the above

Page 17: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Solar & Lunar Eclipses

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Page 18: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Eclipses

• Solar– Moon’s shadow

falls on Earth

• Lunar– Moon moves into

Earth’s shadow

Page 19: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Earth and Moon Shadows

A. Umbra

B. (and C) Penumbra

D. Umbral Extension

Page 20: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Earth and Moon Shadows

A B C D

Appearance

of Sun

Observer location

TotalType of Eclipse Partial Annular

Page 21: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Solar Eclipse

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Page 22: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Lunar EclipseQuickTime™ and aTIFF (Uncompressed) decompressorare needed to see this picture.

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Page 23: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

• When the Moon appears to completely cover the Sun (a solar eclipse), the Moon must be at which phase?

a) fullb) newc) first quarterd) last quarter

Page 24: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

• When the Moon moves through the Earth’s shadow, causing it to appear to darken (a lunar eclipse), the Moon must be at which phase?

a) fullb) newc) first quarterd) last quarter

Page 25: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Motion of the Planets

• Diurnal motion like fixed stars– Rise in “east”– Transit “high/low in south”– Set in “west”

• Position on celestial sphere slowly “slips” from day to day (similar to sun and moon)

Page 26: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Planet Motion

•Generally move from W to E

•Retrograde motion - time when planet appears to move backwards from E to W

E W

Page 27: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Planets

• Planet = Greek for “wanderer”• 5 visible planets (others too faint)

– Mercury, Venus, Mars, Jupiter, Saturn

• Total of 7 wandering objects (including Sun and Moon)

Page 28: Climate and Latitude Sun’s rays –spread over large area = cooler –concentrate in small area = warmer –Warmest where sun directly overhead (at noon) cooler

Planet Location

• Planets always found in Zodiac– 18º wide belt centered on ecliptic

• Mercury and Venus always close to sun• Mars, Jupiter, Saturn seen everywhere (in

Zodiac) – Sometimes near sun (conjunction)– Sometimes opposite to sun (opposition)