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Published byWilliam West Modified over 8 years ago
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The Volcanoes of Io
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Sulfur dioxide As temp increases: white yellow orange brown black
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Sulfur dioxide As temp increases: white yellow orange brown black Volcanoes! ~200 volcanoes Most geologically active body?
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Geologically Active... Internal heat: Left over from formation?
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Geologically Active... Internal heat: Left over from formation? Heat from the Sun?
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Geologically Active... Internal heat: Left over from formation? Heat from the Sun? So where is it coming from...?
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Tidal Heating! 1. Orbital resonances → elliptical orbit
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Tidal Heating! 1. Orbital resonances → elliptical orbit 2. Io is a BIG MOON
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Tidal Heating! 1. Orbital resonances → elliptical orbit 2. Io is a BIG MOON 3. Jupiter is MASSIVE → large gravitational force
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Tidal Heating! 1. Orbital resonances → elliptical orbit 2. Io is a BIG MOON 3. Jupiter is MASSIVE → large gravitational force
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Tidal Heating! 1. Orbital resonances → elliptical orbit 2. Io is a BIG MOON 3. Jupiter is MASSIVE → large gravitational force (what if Io was tiny?) (what if Europa and Ganymede weren't there?)
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Studying Io and its Volcanoes Optical light 5.2 AU → 4% of sunlight Earth receives
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Studying Io and its Volcanoes Optical light 5.2 AU → 4% of sunlight Earth receives Night vision goggles! (Infrared light)
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Studying Io and its Volcanoes Optical light 5.2 AU → 4% of sunlight Earth receives Night vision goggles! (Infrared light) Higher temperature Lower temperature Wavelength tells us something about temperature...
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Blackbody Radiation What gives off blackbody radiation? Stars, planets, light bulbs, stoves, fire, people, etc
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Blackbody Radiation Wavelength: micrometers (0.000001 meters) Temperature: Kelvins (300 K is ~70F) Always positive!
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Blackbody Radiation Total energy emitted is proportional to T 4 Wein's Law: Wavelength * T = 3670
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