Difference between revisions of "Terraforming"

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Presently, [[water|ice]] on Mars [[sublimation|sublimes]] as the atmospheric pressure is so low, ice bypasses the liquid phase when heated. Sublimation occurs allowing ice to turn directly into gas (steam). One of the main challenges for future terraforming efforts would be to increase the atmospheric pressure significantly so water can exist as a liquid on the surface of Mars. The atmospheric pressure will therefore need to be greater than the [[triple point]] of water (thereby existing as ice, liquid and gas).  
 
Presently, [[water|ice]] on Mars [[sublimation|sublimes]] as the atmospheric pressure is so low, ice bypasses the liquid phase when heated. Sublimation occurs allowing ice to turn directly into gas (steam). One of the main challenges for future terraforming efforts would be to increase the atmospheric pressure significantly so water can exist as a liquid on the surface of Mars. The atmospheric pressure will therefore need to be greater than the [[triple point]] of water (thereby existing as ice, liquid and gas).  
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==Short term means==
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A means to do a short term terraforming on Mars can be the [[Bringing down Phobos|bringing down of Phobos]], which certainly releases a great amount of water vapour into the atmosphere.
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==Long term prospect==
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The ultimate results of terraforming are disputed. Terraforming may have only a temporary effect, even if the effect lasts for some hundred or thousand years. Eventually, the [[solar wind]] may carry away most of the new atmosphere due to the insufficient magnetic fields of Mars. Anyway, terraforming Mars can help to give colonization a start.
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[[category:Terraforming Mars]]  
 
[[category:Terraforming Mars]]  
 
[[category:climate]]  
 
[[category:climate]]  
 
[[category:settlements]]
 
[[category:settlements]]

Revision as of 03:16, 12 November 2007

Terraforming, or Earth-shaping, is a theoretical process of modifying a planet's atmosphere to make it habitable for humans. In the case of Mars, terraforming would require artificial thickening of the atmosphere to intensify the process of greenhouse warming (heating the frozen landscape), ice melting to increase the H2O content of the atmosphere (creating water clouds) and greatly increasing the O2 density to ultimately make the atmosphere breathable.

Mars and the "Triple Point" of water

The phase diagram for water, clearly displaying water's triple point.

Presently, ice on Mars sublimes as the atmospheric pressure is so low, ice bypasses the liquid phase when heated. Sublimation occurs allowing ice to turn directly into gas (steam). One of the main challenges for future terraforming efforts would be to increase the atmospheric pressure significantly so water can exist as a liquid on the surface of Mars. The atmospheric pressure will therefore need to be greater than the triple point of water (thereby existing as ice, liquid and gas).

Short term means

A means to do a short term terraforming on Mars can be the bringing down of Phobos, which certainly releases a great amount of water vapour into the atmosphere.

Long term prospect

The ultimate results of terraforming are disputed. Terraforming may have only a temporary effect, even if the effect lasts for some hundred or thousand years. Eventually, the solar wind may carry away most of the new atmosphere due to the insufficient magnetic fields of Mars. Anyway, terraforming Mars can help to give colonization a start.