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Why Mars Died, and Earth Lived

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The Mars rover, Curiosity, is the latest in a long line of missions to Mars
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Landers sent to scoop its soil and study its rocks, orbiters sent to map its valleys and
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ridges.
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They are all asking the same question.
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Did liquid water once flow on this dry and dusty world? Did it support life in any form?
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And are there remnants left to find?
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The science that comes out of these missions may help answer a much larger, more philosophical
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question
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Is our planet Earth the norm, in a galaxy run through with life-bearing planets?
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Or is Earth a rare gem, with a unique make-up and history that allowed it to give rise to
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living things?
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On Mars, Curiosity has spotted pebbles and other rocks commonly associated with flowing
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water.
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It found them down stream on what appears to be an ancient river fan, where water flowed
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down into Gale Crater.
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This shows that at some point in the past, Mars had an atmosphere, cloudy skies, and
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liquid water flowing.
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So what could have turned it into the desolate world we know today?
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One process that very likely played a role goes by the unscientific name, “sputtering.”
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Like the other planets in our solar system, Mars is lashed by high-energy photons from
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the Sun.
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When one of these photons enters the atmosphere of a planet, it can crash into a molecule,
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knocking loose an electron and turning it into an ion.
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The solar wind brings something else: a giant magnetic field.
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When part of the field grazes the planet, it can attract ions and launch them out into
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space.
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Another part might fling ions right into the atmosphere at up to a thousand kilometers
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per second.
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The ions crash into other molecules, sending them in all directions like balls in a game
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of pool.
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Over billions of years, this process could have literally stripped Mars of its atmosphere,
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especially in the early life of the solar system when the solar wind was more intense
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than it is today.
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Sputtering has actually been spotted directly on another dead planet, Venus.
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The Venus Express mission found that solar winds are steadily stripping off lighter molecules
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of hydrogen and oxygen.
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They escape the planet on the night side, then ride solar breezes on out into space.
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This process has left Venus with an atmosphere dominated by carbon dioxide gas, a heat trapping
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compound that has helped send surface temperatures up to around 400 degrees Celsius.
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The loss of Venusatmosphere likely took place over millions of years, especially during
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solar outbursts known as coronal mass ejections.
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If these massive blast waves stripped Venus and Mars of an atmosphere capable of supporting
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lifehow did Earth avoid the same grim fate?
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We can see the answer as the solar storm approaches earth.
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  Our planet has what Mars and Venus lack - a
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powerful magnetic field generated deep within its core.
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  This protective shield deflects many of the
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high-energy particles launched by the Sun.
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In fact, thats just our first line of defense.  
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Much of the solar energy that gets through is reflected back to space by clouds, ice,
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