geol 3045: planetary geology lysa chizmadia saturn lysa chizmadia saturn

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GEOL 3045: Planetary Geology Lysa Chizmadia Saturn

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Page 1: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

GEOL 3045: Planetary GeologyGEOL 3045: Planetary Geology

Lysa ChizmadiaSaturn

Lysa ChizmadiaSaturn

Page 2: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

IntroductionIntroduction 2nd largest planet

– Sixth from Sun (or seventh) Eccentricity = 0.056

– 9.0 - 10.1 AU Axial Tilt = 25.3º

– Earth = 23.5º Orbital period = 29.5 years Rotational period = 10.2 hours (2nd fastest) Mass = 5.69 x 1026 kg

– ~95 Earths Volume = 8.27 x 1014 km3

– ~763 Earths Average = 0.69 g/cm3

= 5.52 g/cm3 (lowest density in solar system) At least 63 moons

2nd largest planet– Sixth from Sun (or seventh)

Eccentricity = 0.056– 9.0 - 10.1 AU

Axial Tilt = 25.3º– Earth = 23.5º

Orbital period = 29.5 years Rotational period = 10.2 hours (2nd fastest) Mass = 5.69 x 1026 kg

– ~95 Earths Volume = 8.27 x 1014 km3

– ~763 Earths Average = 0.69 g/cm3

= 5.52 g/cm3 (lowest density in solar system) At least 63 moons

Image from: http://en.wikipedia.org/wiki/Saturn

Image from: http://www.nineplanets.org/saturn.html

Page 3: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

Internal StructureInternal Structure Atmosphere (59.5 km):

– ~93% H & ~7% He Depleted in He relative to solar

Molecular Hydrogen upper mantle– >100,000 bars– Earth atmosphere ~1 bar

Metallic Hydrogen lower mantle– >1,000,000 bars– Liquid H lower mantle

H nuclei do not have lattice order

Rocky-Ice Core:– 9-22 x Earth

Atmosphere (59.5 km):– ~93% H & ~7% He

Depleted in He relative to solar

Molecular Hydrogen upper mantle– >100,000 bars– Earth atmosphere ~1 bar

Metallic Hydrogen lower mantle– >1,000,000 bars– Liquid H lower mantle

H nuclei do not have lattice order

Rocky-Ice Core:– 9-22 x Earth

Image from: http://solarviews.com/eng/saturn.htm

Page 4: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

AtmosphereAtmosphere Structure:

– Upper clouds: NH3 crystals

– Lower clouds: NH4SH and H2O

Winds among the highest in Solar System– < 500 m/s (~1800 km/h)

Northern hemisphere blue ~ Uranus

With trace amounts of: NH3, C2H2, C2H6, PH3, CH4

Structure:– Upper clouds: NH3 crystals

– Lower clouds: NH4SH and H2O

Winds among the highest in Solar System– < 500 m/s (~1800 km/h)

Northern hemisphere blue ~ Uranus

With trace amounts of: NH3, C2H2, C2H6, PH3, CH4

Image from: http://en.wikipedia.org/wiki/Saturn

Hexagonal Cloud Rotation in N pole

Image from: http://www.solarviews.com/eng/saturn.htm

True color of N pole

Page 5: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

CloudsClouds Ices in clouds:

– H2O, NH3, NH4SH Similar to Jupiter

– Average cloud T: - 185ºC Colder than Jupiter

Bands due to circulation zones– Tropical zones– Wider than Jupiter

Winds up to 500 m/s Great White Spot:

– Occurs once every Saturnian year ~ every 30 y

– Next one in 2020

Ices in clouds:– H2O, NH3, NH4SH

Similar to Jupiter

– Average cloud T: - 185ºC Colder than Jupiter

Bands due to circulation zones– Tropical zones– Wider than Jupiter

Winds up to 500 m/s Great White Spot:

– Occurs once every Saturnian year ~ every 30 y

– Next one in 2020Image from: http://www.solarviews.com/eng/saturn.htm

Image from: http://www.nineplanets.org/saturn.html

Page 6: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

RingsRings Brightest of gas giants Discovered in 1610 by

Galileo Structure:

– <1 km thick

Brightest of gas giants Discovered in 1610 by

Galileo Structure:

– <1 km thick

Images from: http://en.wikipedia.org/wiki/Saturn

Spokes in Rings

Ring over Titan & Enceladus

Image from: http://www.solarviews.com/eng/saturn.htm

Rings edge-on

Image from: http://www.nineplanets.org/saturn.html

Page 7: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

MagnetosphereMagnetosphere ~ magnitude of Earth’s

– 1/20th of Jupiter’s Simple dipole Extends slightly past

orbit of Titan– 1.22 x 106 km

Probably produced by currents in liquid metallic H

~ magnitude of Earth’s – 1/20th of Jupiter’s

Simple dipole Extends slightly past

orbit of Titan– 1.22 x 106 km

Probably produced by currents in liquid metallic H

Saturnian auroral emissions

Image from: http://www.solarviews.com/eng/saturn.htm

Page 8: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

Heat OutputHeat Output Radiates more Q than

receives from Sun– Due to contraction (shrinks

~2 cm/yr)– He raining out of the

atmosphere N hemisphere twice as hot

as S hemisphere

Radiates more Q than receives from Sun– Due to contraction (shrinks

~2 cm/yr)– He raining out of the

atmosphere N hemisphere twice as hot

as S hemisphere

Image from: http://www.solarviews.com/eng/saturn.htm

Thermal view of Saturn

Image from: http://en.wikipedia.org/wiki/Saturn

Thermal emissions

Page 9: GEOL 3045: Planetary Geology Lysa Chizmadia Saturn Lysa Chizmadia Saturn

SummarySummary 2nd largest planet in solar system

– Very fast rotation (day) Atmosphere has fastest winds in solar

system Interior P & T high

– Liquid metallic H mantle Rings have high albedo = icy dust Radiates more heat than receives from

Sun– Due to contraction & He rain– N hemisphere hotter than S hemisphere

2nd largest planet in solar system– Very fast rotation (day)

Atmosphere has fastest winds in solar system

Interior P & T high– Liquid metallic H mantle

Rings have high albedo = icy dust Radiates more heat than receives from

Sun– Due to contraction & He rain– N hemisphere hotter than S hemisphere