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Mars Astronomy 311 Professor Lee Carkner Lecture 14
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Moon Impactor Exercise My data: height = 50 cm = 0.5 m crater diameter = 7 cm mass of marble = 22.4 g = 0.0224 kg Energy PE = mgh = (0.0224)(9.8)(0.5) = 0.11 J Velocity v = (2gh) ½ = [(2)(9.8)(0.5)] ½ = 3.13 m/s Energy-crater size relationship energy/crater size = 0.11 J / 7 cm = 0.016 J/cm for every 0.016 J of energy in your impact the crater size increases by 1 cm Does not seem to hold for any height
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Quiz #2 on Friday Quiz 2 similar format as Quiz 1 ~20 multiple choice/matching ~4 short answer Covers lectures 9-15 bring pencil and calculator Study guide on web page Jupiter observations due Wednesday
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Mars -- The God of War Shows color more strongly than other planets
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The Canals of Mars He called them canali, Italian for “channels” Percival Lowell built an observatory near Flagstaff, AZ and published elaborate maps of a network of canals and oasis on Mars Mars was thought to be very dry, so naturally the inhabitants needed to carefully manage water
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Mars Facts Size: ~1/2 Earth size Orbit: 1.5 AU Description: red, dusty, thin atmosphere
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Spacecraft to Mars Viking 1 and 2 (1975) extensively imaged Mars and also sent landers to the surface Recent missions: Spirit and Opportunity (2003, rover) Phoenix (2008, lander)
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Surface Features Volcanoes -- Mars has many shield volcanoes, but they are not active today Canyons -- Mars shows deep canyons, the result of volcanic activity stressing the crust Craters --The northern hemisphere is less heavily cratered than the southern Why? Dust storms alter the Martian craters
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The Surface of Mars Red dust in atmosphere gives sky a pink tint Surface is covered with reddish soil and is rocky and broken
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Temperature of Mars T M = [R S /(2 D S )] ½ T S Assumes that Mars absorbs all sunlight incident upon it and then radiates the energy freely back into space Mars is cold Mars has seasons due to the tilt of its axis
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Mars’s Atmosphere Pressure: 0.007 atmospheres Early Mars may have had a thicker CO 2 and H 2 O atmosphere Mars has no plate tectonics to return the CO 2 to the atmosphere
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Volatiles on Mars Water cannot exist on the surface of Mars as liquid Even though it is very cold, the low atmospheric pressure makes it easy for water to “escape” the liquid form into a gas Carbon dioxide frost
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Was Mars Wet? Surface features indicate that water once flowed freely on the Martian surface Due to: Spot flooding (water frozen underground and sometimes comes to the surface)? Most likely due to a greenhouse effect Where could the water be now? In the polar caps Mars may warm up periodically allowing water to form (Mars may now be in an ice age)
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Life on Mars? Could life have formed on Mars when it was wetter? Could that life have survived? If life was microscopic it might be hard to find
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Mars’s Interior Mars has a lower density than the other terrestrial planets (4000 compared to 5000 kg/m 3 ) No evidence for plate tectonics There are no seismometers on Mars Mars may have only a small solid iron core or no iron core at all
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Future Mars Exploration large, long-duration rover MAVEN (Mars Atmosphere and Volatile EvolutioN) orbiter planed for 2013 Sample return? Manned mission?
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A Possible History of Mars Mars forms Volcanism creates volcanoes and lava flows Mars losses internal heat, crust cools Atmosphere loses CO 2, atmosphere cools Lava flows stop
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Next Time Read Chapter 14.1 and 14.4
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Summary Red, dusty, thin atmosphere Mars is a medium-sized world allowing it to retain an atmosphere (unlike Mercury and the Moon), but not a thick atmosphere (like Venus and Earth) Mars shows signs of being habitable in the past, but no good evidence of life has been found
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Summary: Surface Mars has a red surface composed of dust, soil and rocks Mars has large volcanoes and deep chasms Dust storms often cover the surface Mars has a low density and may not have an iron core
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Summary: Climate Mars has a very thin atmosphere and is cold Low temperature and pressure prevent liquid water on the surface Mars may have had a thicker, warmer atmosphere in the past since there is substantial evidence for water flows Early thicker CO 2 greenhouse atmosphere gradually washed out by rainfall The temperature on Mars may change over time due to orbital variations
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