logging in or signing up 16 Atmospheric Evolution Teobaldo Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 579 Category: Education License: All Rights Reserved Like it (0) Dislike it (0) Added: January 25, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Atmospheric Evolution of Earth, Venus and MarsMar’s Moons & Life on Mars: Atmospheric Evolution of Earth, Venus and Mars Mar’s Moons & Life on Mars Leonard Garcia Linda Phan, Dennis Huynh Group 16Atmospheric Evolution of the Earth: Atmospheric Evolution of the EarthPrimary AtmosphereGas, Poison, and a Whole lot of Heat: Primary Atmosphere Gas, Poison, and a Whole lot of Heat Most likely resembled that of Jupiter's atmosphere Contained hydrogen, helium, methane, ammonia, water vapor Poisonous to humansOutgassingGassing it Out: Outgassing Gassing it Out Volcanic activity Released water vapor, carbon dioxide, sulfur dioxide, and compounds containing nitrogen into atmosphere Secondary AtmosphereFinally beginning to cool down: Secondary Atmosphere Finally beginning to cool down Surface Temperature dropped Carbon dioxide and sulfur dioxide dissolved into oceans or combined with surface rocks Water vapor condensed – oceans BUT still no oxygenIT’S ALIVE!!Life and oxygen: IT’S ALIVE!! Life and oxygen Life developed in the oceans Organisms began producing oxygen Ozone layer formed, life moved to landTO REVIEW: TO REVIEW Outgassing N2 CO2 H2O oceans form CO2 dissolves Life forms in oceans Onset of photosynthesis O2 O2 reaches current levels; life invades continents 4.5 Gy B.P 4 Gy B.P. 3.5 Gy B.P. 0.4 Gy B.P. presentRunaway Greenhouse EffectWhy is Venus so Hot? : Runaway Greenhouse Effect Why is Venus so Hot? 730 K Surface TemperatureGreenhouse GasesThe second blanket: Greenhouse Gases The second blanket Greenhouse gases stop the escape of infrared radiation emitted by a planet’s surface Carbon dioxide and water vapor are Greenhouse Gases Venus’ atmosphere consists of nearly 96 percent Carbon dioxideThe Runaway Greenhouse EffectGetting a bit out of hand…: The Runaway Greenhouse Effect Getting a bit out of hand… In the past, Venus’ water vapors made the surface temperature twice as hot as it is today Water vapor reached the upper atmosphere at these temperatures and was broken up into oxygen and hydrogen by solar UV radiation Hydrogen escaped into space No more water on VenusEvolution of the Martian Atmosphere: Evolution of the Martian Atmosphere Believed to have started off much like earth, with a primary and a secondary atmosphere Greenhouse effect would have kept Mars warmWhy did the Martian Atmosphere Disappear?: Why did the Martian Atmosphere Disappear? Possibly because of large impacts early in the solar system’s development Gases could have leaked into space because of Mar’s weak gravitational pullReverse Runaway Greenhouse Effect: Reverse Runaway Greenhouse Effect Carbon dioxide combined with surface rocks and dissolved into water Decrease of carbon dioxide caused Mars to cool down, freezing any water it hadThe Moons of MarsFear and Panic: The Moons of Mars Fear and Panic Discovered in 1877 by Asaph Hall. Deimos (Panic) is 16 km long & 10 km wide. Phobos (Fear) is 28 km long & 20 km wide.Asteroids from the belt: Asteroids from the belt These moons are asteroids that were captured by Mars’ atmosphere. It is possible that the two moons are remnants of a single object that split during capture. Life on Mars?: Life on Mars? Lack of liquid water and oxygen dims the chances that there might be life on Mars Water in Mar’s history might have provided an environment suitable for life at one time, thoughA Machine on MarsViking sent to do the dirty work: A Machine on Mars Viking sent to do the dirty work Viking missions reached Mars in 1976 Viking performed various biological experiments on the soil on mars The tests initially suggested life on Mars, but scientists pointed out that the tests could have been the result of inorganic chemical reactions Official NASA Statement said there is no life on MarsOk, no life on Mars, but what about a billion years ago?: Ok, no life on Mars, but what about a billion years ago? Scientists want to launch more missions to test ice caps for fossils Meteoroids from Mars found on Earth have been tested for fossilized remains There are remains, but scientists suggest these may be Earth bacteria fossils The question of Life on Mars remains inconclusive You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
16 Atmospheric Evolution Teobaldo Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 579 Category: Education License: All Rights Reserved Like it (0) Dislike it (0) Added: January 25, 2008 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Atmospheric Evolution of Earth, Venus and MarsMar’s Moons & Life on Mars: Atmospheric Evolution of Earth, Venus and Mars Mar’s Moons & Life on Mars Leonard Garcia Linda Phan, Dennis Huynh Group 16Atmospheric Evolution of the Earth: Atmospheric Evolution of the EarthPrimary AtmosphereGas, Poison, and a Whole lot of Heat: Primary Atmosphere Gas, Poison, and a Whole lot of Heat Most likely resembled that of Jupiter's atmosphere Contained hydrogen, helium, methane, ammonia, water vapor Poisonous to humansOutgassingGassing it Out: Outgassing Gassing it Out Volcanic activity Released water vapor, carbon dioxide, sulfur dioxide, and compounds containing nitrogen into atmosphere Secondary AtmosphereFinally beginning to cool down: Secondary Atmosphere Finally beginning to cool down Surface Temperature dropped Carbon dioxide and sulfur dioxide dissolved into oceans or combined with surface rocks Water vapor condensed – oceans BUT still no oxygenIT’S ALIVE!!Life and oxygen: IT’S ALIVE!! Life and oxygen Life developed in the oceans Organisms began producing oxygen Ozone layer formed, life moved to landTO REVIEW: TO REVIEW Outgassing N2 CO2 H2O oceans form CO2 dissolves Life forms in oceans Onset of photosynthesis O2 O2 reaches current levels; life invades continents 4.5 Gy B.P 4 Gy B.P. 3.5 Gy B.P. 0.4 Gy B.P. presentRunaway Greenhouse EffectWhy is Venus so Hot? : Runaway Greenhouse Effect Why is Venus so Hot? 730 K Surface TemperatureGreenhouse GasesThe second blanket: Greenhouse Gases The second blanket Greenhouse gases stop the escape of infrared radiation emitted by a planet’s surface Carbon dioxide and water vapor are Greenhouse Gases Venus’ atmosphere consists of nearly 96 percent Carbon dioxideThe Runaway Greenhouse EffectGetting a bit out of hand…: The Runaway Greenhouse Effect Getting a bit out of hand… In the past, Venus’ water vapors made the surface temperature twice as hot as it is today Water vapor reached the upper atmosphere at these temperatures and was broken up into oxygen and hydrogen by solar UV radiation Hydrogen escaped into space No more water on VenusEvolution of the Martian Atmosphere: Evolution of the Martian Atmosphere Believed to have started off much like earth, with a primary and a secondary atmosphere Greenhouse effect would have kept Mars warmWhy did the Martian Atmosphere Disappear?: Why did the Martian Atmosphere Disappear? Possibly because of large impacts early in the solar system’s development Gases could have leaked into space because of Mar’s weak gravitational pullReverse Runaway Greenhouse Effect: Reverse Runaway Greenhouse Effect Carbon dioxide combined with surface rocks and dissolved into water Decrease of carbon dioxide caused Mars to cool down, freezing any water it hadThe Moons of MarsFear and Panic: The Moons of Mars Fear and Panic Discovered in 1877 by Asaph Hall. Deimos (Panic) is 16 km long & 10 km wide. Phobos (Fear) is 28 km long & 20 km wide.Asteroids from the belt: Asteroids from the belt These moons are asteroids that were captured by Mars’ atmosphere. It is possible that the two moons are remnants of a single object that split during capture. Life on Mars?: Life on Mars? Lack of liquid water and oxygen dims the chances that there might be life on Mars Water in Mar’s history might have provided an environment suitable for life at one time, thoughA Machine on MarsViking sent to do the dirty work: A Machine on Mars Viking sent to do the dirty work Viking missions reached Mars in 1976 Viking performed various biological experiments on the soil on mars The tests initially suggested life on Mars, but scientists pointed out that the tests could have been the result of inorganic chemical reactions Official NASA Statement said there is no life on MarsOk, no life on Mars, but what about a billion years ago?: Ok, no life on Mars, but what about a billion years ago? Scientists want to launch more missions to test ice caps for fossils Meteoroids from Mars found on Earth have been tested for fossilized remains There are remains, but scientists suggest these may be Earth bacteria fossils The question of Life on Mars remains inconclusive