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Chapter 3: Earth-Sun Relationships and Solar Energy Physical Physical Geography Geography Ninth Edition Ninth Edition Robert E. Gabler James. F. Petersen L. Michael Trapasso

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Chapter 3: Earth-Sun Relationships and Solar Energy

Physical Physical GeographyGeographyNinth EditionNinth Edition

Robert E. Gabler

James. F. Petersen

L. Michael Trapasso

Dorothy Sack

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3.1 Solar System and Beyond

• Galaxy: enormous cluster of stars, dust, and gases.– Our sun is one of billions of

stars within the Milky way Galaxy

– Vast distances• Other than the sun, our

nearest star is 4.2 light years away

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3.1 Solar System and Beyond

• Solar System• Gravity: attractive force one

body has on another• Mass: the greater the mass, the

greater the gravitational pull.• Planet: celestial body in orbit of

the sun, with sufficient gravitational attraction to overcome rigid forces and remain nearly spherical.

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3.1 Solar System and Beyond

• Our solar system– Satellites (earth’s moons)– Numerous asteroids– Comet: head (collection of

solid fragments held together by ice)

– Meteors: small stonelike, or metallic bodies.

– Meteorite: meteor that survives the fall through our sky.

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3.1 Solar System and Beyond

• The Planets– Terrestrial: 4 closest to the sun

• Mercury, Venus, Earth, and Mars• Solid surfaces

– Gas Planets: 4 furthest from sun• Jupiter, Saturn, Uranus, and Neptune• Huge balls of gas and liquid

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Comparison of the Planets

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3.2 The Earth-Sun System

• Sun and its Energy– Thermonuclear fusion

powers the sun– 2 hydrogen atoms fuse

together to form 1 helium atom.

– Photosphere– Chromosphere– Corona

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3.2 The Earth-Sun System

• Solar wind: directed toward the magnetic poles.

• This forms an aurora– Northern lights (Aurora

Borealis)– Southern lights (Aurora

Australis)

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Aurora Borealis

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3.2 The Earth-Sun System

• Sunspots: intensity of solar winds

• Next cycle should peak around the year 2012.

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3.2 The Earth-Sun System

• Solar Energy and Atmospheric Dynamics– energy emitted from the

sun is in the form of Electromagnetic energy.

– Shortwave (SW) radiation– Longwave (LW) radiation:

energy that may have been emitted from earth.

– Solar constant

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3.2 The Earth-Sun System

• Movements of Earth– Galactic movement– Rotation– revolution

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3.2 The Earth-Sun System

• Rotation– Earth turns eastward – Counterclockwise spin

on its axis– 24 hours per rotation– Speed is fastest at the

equator.

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Circle of Illumination

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3.2 The Earth-Sun System

• Revolution– Slightly elliptical orbit– Closest to sun near Jan.

3rd (perihelion)– Furthest from sun

around July 4th (aphelion)

– This has minimal affect on the energy receipt on earth

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3.2 The Earth-Sun System

• Plane of the ecliptic– Earth is titled at 23.5

degrees. – angle of inclination

• Parallelism: Earth’s axis remains parallel to its former position.

• These positions change slowly over time (Milankovitch cycles)

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3.3 Sun Angle, Duration, and Insolation

• Insolation: Solar radiation received by Earth.– Main source of energy on

our planet– Seasonal variations in

temperature due primarily to fluctuations in insolation

– Direct rays– Oblique rays

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3.3 Sun Angle, Duration, and Insolation

Direct rays at 23.5o N Direct rays at equator

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3.3 Sun Angle, Duration, and Insolation

• The Seasons– Summer Solstice (~ June 21) in N. hemisphere

• Direct rays at 23.5o N (Tropic of Cancer)• Northern hemisphere receives more energy• 24 hours of sunlight (Arctic Circle to North Pole)• Longest day of the year in N. hem. • Shortest day of the year in S. hem.

– Autumnal Equinox in (~ Sept. 22) N. hem.• Direct rays at equator• 12 hours of daylight everywhere

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3.3 Sun Angle, Duration, and Insolation

• The Seasons– Winter Solstice (~ Dec. 21) in N. hemisphere

• Direct rays at 23.5o S (Tropic of Capricorn)• Southern hemisphere receives more energy• 24 hours of sunlight (Antarctic Circle to South Pole)• Shortest day of the year in N. hem. • Longest day of the year in S. hem.

– Vernal Equinox in (~ March 20) N. hem.• Direct rays at equator• 12 hours of daylight everywhere

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The Seasons (Focus on Solstices)

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The Seasons (Focus on Equinox)

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Duration of daylight for certain Latitudes

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3.3 Sun Angle, Duration, and Insolation

• Sun’s declination: Latitude at which the sun is directly overhead

• Analemma: Shows the sun’s declination throughout the year.

• What is the declination on Oct 10th?

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3.3 Sun Angle, Duration, and Insolation

• Variations of Insolation with Latitude– Tropical Zones– Middle latitude zones– Polar zones

• Which zone(s) would have the least annual variation?

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Ancient Civilizations (Mayan Pyramid)

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Physical Geography

End of Chapter 3: Earth-Sun Relationships and Solar Energy